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  • image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    Authors: Aaboud, M; Aad, G; Abbott, B; Abdallah, J; +196 Authors

    With the increase in energy of the Large Hadron Collider to a centre-of-mass energy of 13 TeV for Run 2, events with dense environments, such as in the cores of high-energy jets, became a focus for new physics searches as well as measurements of the Standard Model. These environments are characterized by charged-particle separations of the order of the tracking detectors sensor granularity. Basic track quantities are compared between 3.2 fb$^{-1}$ of data collected by the ATLAS experiment and simulation of proton-proton collisions producing high-transverse-momentum jets at a centre-of-mass energy of 13 TeV. The impact of charged-particle separations and multiplicities on the track reconstruction performance is discussed. The efficiency in the cores of jets with transverse momenta between 200 GeV and 1600 GeV is quantified using a novel, data-driven, method. The method uses the energy loss, dE/dx, to identify pixel clusters originating from two charged particles. Of the charged particles creating these clusters, the measured fraction that fail to be reconstructed is $0.061 \pm 0.006 \textrm{(stat.)} \pm 0.014 \textrm{(syst.)}$ and $0.093 \pm 0.017 \textrm{(stat.)}\pm 0.021 \textrm{(syst.)}$ for jet transverse momenta of 200-400 GeV and 1400-1600 GeV, respectively. The European physical journal / C 77(10), 673 (2017). doi:10.1140/epjc/s10052-017-5225-7 Published by Springer, Berlin

    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/ COREarrow_drop_down
    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    CORE
    Article . 2017
    License: CC BY
    Data sources: CORE
    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    PubMed Central
    Other literature type . 2017
    Data sources: PubMed Central
    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    HAL-UPMC
    Article . 2017
    License: CC BY
    Data sources: HAL-UPMC
    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    HAL Clermont Université
    Article . 2017
    License: CC BY
    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    HAL AMU
    Article . 2017
    License: CC BY
    Data sources: HAL AMU
    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    HAL-CEA
    Article . 2017
    License: CC BY
    Data sources: HAL-CEA
    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    CERN Document Server
    Other literature type . 2017
    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
    image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
    image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
    image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
    image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
    image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
    image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
    https://dx.doi.org/10.48550/ar...
    Article . 2017
    License: arXiv Non-Exclusive Distribution
    Data sources: Datacite
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    This Research product is the result of merged Research products in OpenAIRE.

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      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/ COREarrow_drop_down
      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
      CORE
      Article . 2017
      License: CC BY
      Data sources: CORE
      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
      PubMed Central
      Other literature type . 2017
      Data sources: PubMed Central
      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
      HAL-UPMC
      Article . 2017
      License: CC BY
      Data sources: HAL-UPMC
      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
      HAL Clermont Université
      Article . 2017
      License: CC BY
      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
      HAL AMU
      Article . 2017
      License: CC BY
      Data sources: HAL AMU
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      https://dx.doi.org/10.48550/ar...
      Article . 2017
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  • Authors: Peng Liu; Shu Ting Dong; Bin Zhao; Dan Dan Hu; +1 Authors

    To explore the effects of different densities of mixed-cropping on 13C-photosynthate distribution and grain yield of maize, we measured photosynthetic characteristics, 13C-photosynthate distribution, dry matter accumulation, and grain yield under different planting densities (LD, 67500 plants·hm-2 and HD, 97500 plants·hm-2) under mixed-cropping (M, 1:1, 2:2) and monoculture of Zhengdan958 (ZD) and Denghai605 (DH). The results showed that with the increases of planting density, grain yield, 13C-photosynthate allocation to grain, dry matter accumulation, and leaf area index (LAI) increased, but the chlorophyll content and net photosynthetic rate decreased. No significant difference was observed between the monoculture and mixed-cropping at the density of 67500 plants·hm-2. However, at 97500 plants·hm-2, LAI, chlorophyll content, net photosynthetic rate and dry matter accumulation in mixed-cropping were higher than that in monoculture. Mixed-cropping promoted the transport of dry matter from the vegetative organs such as stem to the grain and the distribution of 13C-photosynthates to grain. Grain yield of summer maize significantly increased in mixed-cropping due to the increase of 1000-grain mass. Under high plant density, the mixed-cropping could enlarge photosynthetic area, maintain higher net photosynthetic rate, increase dry matter accumulation, improve the distribution of dry matter, promote the distribution of 13C-photosynthates to grains and thus increase the grain yield. Our results indicated that mixed-cropping could significantly increase the yield of close planting summer maize in Huang-Huai-Hai Plain.

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  • Authors: Hairu Jin; Jian Zhuge; Huiying Fang;

    Candida glycerinogenes is an aerobe which does not depend on sulphite for production of glycerol. With a sufficient O2 supply, up to 130 g glycerol l(-1) was produced with 2.6 g acetic acid l(-1) as by-product. However, with an insufficient O2 supply--with higher volumes of medium or at higher corn steep liquid concentrations--the glycerol concentration was lower because the by-products, ethanol, pyruvate and lactic acid, were produced in greater amounts, up to 45 g l(-1), 4.3 g l(-1), 1.6 g l(-1), respectively, whereas, less acetic acid (0.6 g l(-1)) was produced. In addition, ethanol decreased to 0.4 g l(-1) and the glycerol yield improved from 34 to 50% (w/w) by adding 50 g sulphite l(-1), nevertheless, acetic acid increased to 7.8 g l(-1).

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  • Authors: Kai Ning; Pei-Xin Zhang; Zhen-Jing Yang; Xian-Zhe Dong; +2 Authors

    The Quaternary sediment in the Ningbo Coastal Plain was the deposit due to sea-land interaction, which recorded information of past climate changes. The region is therefore an ideal area to study paleoclimate changes and sedimentary characteristics. We determined the stratigraphic division and paleoenvironmental evolution based on 14C and paleomagnetic dating, along with detailed analyses of lithology, pollen assemblage, foraminifera and ostracodes assemblage, and grain size of sediment in core Z02 located in the southeastern Ningbo Coastal Plain. The results showed that the boundary between the Holocene and Upper Pleistocene in the core Z02 record was at 30.5 m, the boundary between the Upper and Middle Pleistocene was at 82.65 m, and the boundary between the Quaternary and Lower Cretaceous was at 90 m. The Middle Pleistocene section of the core contained few sediments, while the Lower Pleistocene section was completely missed. During the late Pleistocene, the hydrodynamic conditions experienced energy levels of medium to medium low to medium, and sedimentary facies changed from alluvial lake to overbank to river to lake to alluvial lake to lake to overbank. During the Holocene, the hydrodynamic changes experienced energy levels of medium low to low to medium, and the sedimentary facies changed from shoreland to shallow sea to shoreland lake. The Ningbo Coastal Plain had experienced tectonic uplift, weathering and erosion stage in the Early and Middle Pleistocene, from warm and humid to dry in the Late Pleistocene, and from warm and humid to dry and cool in the Holocene, as revealed by the core Z02 record. This study provided useful information in investigating past environmental changes in the subtropical coastal region of eastern China.

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    Authors: Cai, Ruohong; Yu, Danlin; Oppenheimer, Michael; Cai, Ruohong; +2 Authors

    Researchers have extensively studied crop yield response to weather variations, while only a limited number of studies have attempted to identify spatial heterogeneity in this relationship. We explore spatial heterogeneity in corn yield response to weather by combining geographically weighted regression and panel regression. We find that temperature tends to have negative effects on U.S. corn yields in warmer regions and positive effects in cooler regions, with spatial heterogeneity at a fine scale. The spatial pattern of precipitation effects is more complicated. A further analysis shows that precipitation effects are sensitive to the existence of irrigation systems.

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    https://dx.doi.org/10.22004/ag...
    Other literature type . 2014
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      https://dx.doi.org/10.22004/ag...
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    Authors: Vitalina Babenko; Miroshnichenko Tetyana; Dmytro Zherlitsyn; Olena Dovgal; +2 Authors

    The processes of transformation of the energy space, namely the impact of alternative energy resources on it, are characterized by changes in the national economy in general and in the energy market in particular. The results of the analysis confirmed the significant dependence of electricity production indicators on renewable sources and such factors as GDP, CO2 emissions, total electricity production, which requires improvement of organizational and economic bases for policy development of state support for renewable energy technologies in countries with exogenous factors. The interdependence between electricity production from renewable sources and economic indicators in Ukrainian-Chilean relations using macroeconomic multifactor analysis based on the correlation method allowed to identify the most influential factors.

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    Authors: Tong, Shi Lu; Olsen, Jorn; Kinney, Patrick L.;
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    Résumé. L'émission biogénique d'oxyde nitrique (NO) du sol a un impact important sur un certain nombre de questions environnementales, telles que la production d'ozone troposphérique, le cycle du radical hydroxyle (OH) et la production de NO. Dans cette étude, nous avons collecté les sols de quatre types de parcelles de végétation différents (pan, prairie annuelle, prairie vivace et brousse empiétée) dans un écosystème de savane aride du Kalahari (Botswana). Une technique d'incubation en laboratoire a été utilisée pour déterminer le flux net potentiel de NO des sols en fonction de l'humidité du sol et de la température du sol. Les émissions potentielles nettes de NO ont été augmentées pour l'année 2006 et une région (185 km×185 km) du sud du Kalahari. Pour cela, nous avons utilisé (a) les émissions potentielles nettes de NO mesurées en laboratoire, (b) la distribution des parcelles de végétation obtenue à partir des mesures NDVI de Landsat, (c) les teneurs en humidité du sol estimées obtenues à partir des mesures ENVISAT ASAR et (d) la température de surface du sol estimée à l'aide des mesures de température de surface MODIS MOD11A2 sur 8 jours. Les différences dans les flux de NO potentiels nets entre les parcelles de végétation se produisent et vont de 0,27 ng m−2 s−1 dans les parcelles de Pan à 2,95 ng m−2 s−1 dans les parcelles de prairie vivace. La mise à l'échelle des flux de NO potentiels nets avec les données satellitaires sur l'humidité et la température du sol a donné des flux de NO allant jusqu'à 323 g ha−1 mois−1, où les flux de NO les plus élevés se sont produits dans les parcelles de prairies vivaces et les plus bas dans les parcelles de Pan. Une tendance saisonnière marquée a été observée où les flux les plus élevés se sont produits pendant les mois d'été austral (janvier et février) tandis que les flux minimums se sont produits pendant les mois d'hiver austral (juin et juillet), et étaient inférieurs à 1,8 g ha−1 mois−1. Au cours de l'année, les émissions moyennes de NO pour la région mise à l'échelle étaient de 0,54 kg ha−1 an−1, ce qui représente une perte allant jusqu'à 7,4 % de l'apport d'azote (N) dans la région par les dépôts atmosphériques et la fixation biologique de l'azote. L'émission biogénique de NO du sol est donc un mécanisme important de perte d'azote de cet écosystème de savane aride et a le potentiel de jouer un rôle important dans la production d'ozone troposphérique et le cycle OH. Resumen. La emisión biogénica de óxido nítrico (NO) del suelo tiene un impacto importante en una serie de cuestiones ambientales, como la producción de ozono troposférico, el ciclo del radical hidroxilo (OH) y la producción de NO. En este estudio recolectamos suelos de cuatro tipos diferentes de parches de vegetación (Pan, Annual Grassland, Perennial Grassland y Bush Encroached) en un ecosistema de sabana árida en el Kalahari (Botswana). Se utilizó una técnica de incubación de laboratorio para determinar el flujo de NO potencial neto de los suelos en función de la humedad del suelo y la temperatura del suelo. Las emisiones netas potenciales de NO se aumentaron para el año 2006 y una región (185 km×185 km) del Kalahari meridional. Para ello, utilizamos (a) las emisiones potenciales netas de NO medidas en el laboratorio, (b) la distribución de parches de vegetación obtenida a partir de las mediciones de Landsat NDVI, (c) los contenidos estimados de humedad del suelo obtenidos a partir de las mediciones de ENVISAT asar y (d) la temperatura de la superficie del suelo estimada utilizando las mediciones de temperatura de la superficie terrestre MODIS MOD11A2 de 8 días. Se producen diferencias en el potencial neto de flujos de NO entre parches de vegetación y van desde 0.27 ng m−2 s−1 en los parches de Pan hasta 2.95 ng m−2 s−1 en los parches de pastizales perennes. La ampliación de los flujos de NO potenciales netos con los datos de humedad y temperatura del suelo obtenidos por satélite dio NO flujos de hasta 323 g ha−1 mes−1, donde los mayores flujos de NO aumentados ocurrieron en los parches de pastizales perennes y los más bajos en los parches de pan. Se observó un patrón estacional marcado donde los flujos más altos ocurrieron en los meses de verano australes (enero y febrero) mientras que los flujos mínimos ocurrieron en los meses de invierno australes (junio y julio), y fueron menores a 1.8 g ha−1 mes−1. A lo largo del año, la emisión media de NO para la región aumentada fue de 0,54 kg ha−1 año−1, lo que representa una pérdida de hasta el 7,4% de la entrada de nitrógeno (N) a la región a través de la deposición atmosférica y la fijación biológica de N. La emisión biogénica de NO del suelo es, por lo tanto, un mecanismo importante de pérdida de N de este ecosistema de sabana árida y tiene el potencial de desempeñar un papel importante en la producción de ozono troposférico y el ciclo de OH. Abstract. The biogenic emission of nitric oxide (NO) from the soil has an important impact on a number of environmental issues, such as the production of tropospheric ozone, the cycle of the hydroxyl radical (OH) and the production of NO. In this study we collected soils from four differing vegetation patch types (Pan, Annual Grassland, Perennial Grassland and Bush Encroached) in an arid savanna ecosystem in the Kalahari (Botswana). A laboratory incubation technique was used to determine the net potential NO flux from the soils as a function of the soil moisture and the soil temperature. The net potential NO emissions were up-scaled for the year 2006 and a region (185 km×185 km) of the southern Kalahari. For that we used (a) the net potential NO emissions measured in the laboratory, (b) the vegetation patch distribution obtained from Landsat NDVI measurements, (c) estimated soil moisture contents obtained from ENVISAT ASAR measurements and (d) the soil surface temperature estimated using MODIS MOD11A2 8 day land surface temperature measurements. Differences in the net potential NO fluxes between vegetation patches occur and range from 0.27 ng m−2 s−1 in the Pan patches to 2.95 ng m−2 s−1 in the Perennial Grassland patches. Up-scaling the net potential NO fluxes with the satellite derived soil moisture and temperature data gave NO fluxes of up to 323 g ha−1 month−1, where the highest up-scaled NO fluxes occurred in the Perennial Grassland patches, and the lowest in the Pan patches. A marked seasonal pattern was observed where the highest fluxes occurred in the austral summer months (January and February) while the minimum fluxes occurred in the austral winter months (June and July), and were less than 1.8 g ha−1 month−1. Over the course of the year the mean NO emission for the up-scaled region was 0.54 kg ha−1 yr−1, which accounts for a loss of up to 7.4% of the nitrogen (N) input to the region through atmospheric deposition and biological N fixation. The biogenic emission of NO from the soil is therefore an important mechanism of N loss from this arid savanna ecosystem and has the potential to play an important role in the production of tropospheric ozone and the OH cycle. الخلاصة. للانبعاث الحيوي لأكسيد النيتريك (NO) من التربة تأثير مهم على عدد من القضايا البيئية، مثل إنتاج الأوزون التروبوسفيري، ودورة جذر الهيدروكسيل (OH) وإنتاج NO. في هذه الدراسة جمعنا التربة من أربعة أنواع مختلفة من الرقع النباتية (عموم، المراعي السنوية، المراعي المعمرة وبوش التعدي) في النظام البيئي السافانا القاحلة في كالاهاري (بوتسوانا). تم استخدام تقنية الحضانة المختبرية لتحديد صافي تدفق NO المحتمل من التربة كدالة لرطوبة التربة ودرجة حرارة التربة. تم رفع صافي انبعاثات NO المحتملة لعام 2006 ومنطقة (185 كم×185 كم) من جنوب كالاهاري. لذلك استخدمنا (أ) صافي انبعاثات NO المحتملة المقاسة في المختبر، (ب) توزيع رقعة الغطاء النباتي الذي تم الحصول عليه من قياسات Landsat NDVI، (ج) محتويات رطوبة التربة المقدرة التي تم الحصول عليها من قياسات ENVISAT ASAR و (د) درجة حرارة سطح التربة المقدرة باستخدام قياسات درجة حرارة سطح الأرض MODIS MOD11A2 لمدة 8 أيام. تحدث اختلافات في صافي التدفقات المحتملة بين بقع الغطاء النباتي وتتراوح من 0.27 نانوغرام م -2 ثانية-1 في بقع المقلاة إلى 2.95 نانوغرام م-2 ثانية-1 في بقع المراعي المعمرة. لم ينتج عن زيادة صافي تدفقات NO المحتملة مع بيانات رطوبة التربة ودرجة الحرارة المستمدة من القمر الصناعي أي تدفقات تصل إلى 323 جم هكتار-1 شهر-1، حيث حدثت أعلى تدفقات NO على نطاق واسع في بقع المراعي المعمرة، وأدناها في بقع المقلاة. لوحظ نمط موسمي ملحوظ حيث حدثت أعلى التدفقات في أشهر الصيف الأسترالية (يناير وفبراير) بينما حدث الحد الأدنى من التدفقات في أشهر الشتاء الأسترالية (يونيو ويوليو)، وكانت أقل من 1.8 جم هكتار-1 شهر-1. على مدار العام، كان متوسط انبعاثات NO للمنطقة الصاعدة 0.54 كجم هكتار-1 سنة-1، وهو ما يمثل خسارة تصل إلى 7.4 ٪ من مدخلات النيتروجين (N) إلى المنطقة من خلال الترسب في الغلاف الجوي والتثبيت البيولوجي لـ N. وبالتالي، فإن الانبعاثات الحيوية من NO من التربة هي آلية مهمة لفقدان N من هذا النظام البيئي للسافانا القاحلة ولديها القدرة على لعب دور مهم في إنتاج الأوزون التروبوسفيري ودورة OH.

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    Biogeosciences (BG)
    Other literature type . 2018
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    https://dx.doi.org/10.60692/hr...
    Other literature type . 2008
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  • Authors: Ming-Ming Li; Gang Li;

    Based on 98 Chinese pine (Pinus tabuliformis) tree-ring width data, normalized diffe-rence vegetation index (NDVI) data and land cover data in the Helan Mountains, we used VS-oscilloscope model to simulate the radial growth process of Chinese pine and to examine the relationship between vegetation canopy phenology and tree cambium phenology. Results showed that the end of season (EOS) of the vegetation canopy was significantly correlated with the EOS of the Chinese pine cambium. Such correlation was stronger than that between grassland and cambium. The start of season (SOS) and EOS of Chinese pine were related to the averaged minimum temperature in May-June and August-September, respectively. When the average minimum temperature in May-June increased by 1 ℃, SOS would be advanced by 4.3 days. The averaged minimum temperature in August-September increased by 1 ℃, EOS would be delayed by 2.6 days. The correlation between the phenology of vegetation canopy and the phenology of the cambium in Chinese pine differed among vegetation types. Simulating tree growth dynamics only through a tree-ring physiology model might lead to biased results. Using remote sensing monitoring data to combine canopy development and cambium growth would help to more accurately understand tree growth dynamics.

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  • Authors: Rui Li; Qi-Jie Yang;

    Alsophila spinulosa is a rare and endangered relict fern species. With the Maxent model, we predicted the global potential suitable habitat and its future changes for A. spinulosa. We evaluated the accuracy of our prediction based on the receiver operating characteristic curve (ROC), in order to provide reference for the protection, detection and cultivation of its resources. The results showed that most potential suitable habitat for A. spinulosa would be in Asia and few in North Ame-rica, Central America, Madagascar, La Réunion, Mauritius, Seychelles, New Zealand, New Caledonia and Fiji. The global potential suitable habitat for A. spinulosa under current climate conditions encompassed 357.1×104 km2, with Asia accounting for 88.4% and China for 49.5% of the total. The highly suitable habitat for A. spinulosa in China would be mainly in Yunnan-Guizhou Plateau, Sichuan Basin, south of the Nanling Mountains and Taiwan Island. The critical factors driving the distribution of A. spinulosa would be the precipitation of warmest quarter, July average precipita-tion, temperature seasonality and mean diurnal range. Under the SSP1_2.6 climate scenario, the global potential suitable habitat for A. spinulosa would decrease by 7.8% from 2041 to 2060, and increase by 3.2% from 2081 to 2100. Under the SSP2_4.5 climate scenario, it would increase by 2.9% from 2041 to 2060 and by 7.2% from 2081 to 2100. Under the SSP5_8.5 climate scenario, it would increase by 3.3% from 2041 to 2060 and by 5.3% from 2081 to 2100.

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    Authors: Aaboud, M; Aad, G; Abbott, B; Abdallah, J; +196 Authors

    With the increase in energy of the Large Hadron Collider to a centre-of-mass energy of 13 TeV for Run 2, events with dense environments, such as in the cores of high-energy jets, became a focus for new physics searches as well as measurements of the Standard Model. These environments are characterized by charged-particle separations of the order of the tracking detectors sensor granularity. Basic track quantities are compared between 3.2 fb$^{-1}$ of data collected by the ATLAS experiment and simulation of proton-proton collisions producing high-transverse-momentum jets at a centre-of-mass energy of 13 TeV. The impact of charged-particle separations and multiplicities on the track reconstruction performance is discussed. The efficiency in the cores of jets with transverse momenta between 200 GeV and 1600 GeV is quantified using a novel, data-driven, method. The method uses the energy loss, dE/dx, to identify pixel clusters originating from two charged particles. Of the charged particles creating these clusters, the measured fraction that fail to be reconstructed is $0.061 \pm 0.006 \textrm{(stat.)} \pm 0.014 \textrm{(syst.)}$ and $0.093 \pm 0.017 \textrm{(stat.)}\pm 0.021 \textrm{(syst.)}$ for jet transverse momenta of 200-400 GeV and 1400-1600 GeV, respectively. The European physical journal / C 77(10), 673 (2017). doi:10.1140/epjc/s10052-017-5225-7 Published by Springer, Berlin

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    CORE
    Article . 2017
    License: CC BY
    Data sources: CORE
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    PubMed Central
    Other literature type . 2017
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    HAL-UPMC
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    HAL Clermont Université
    Article . 2017
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    HAL AMU
    Article . 2017
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    CERN Document Server
    Other literature type . 2017
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      https://dx.doi.org/10.48550/ar...
      Article . 2017
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  • Authors: Peng Liu; Shu Ting Dong; Bin Zhao; Dan Dan Hu; +1 Authors

    To explore the effects of different densities of mixed-cropping on 13C-photosynthate distribution and grain yield of maize, we measured photosynthetic characteristics, 13C-photosynthate distribution, dry matter accumulation, and grain yield under different planting densities (LD, 67500 plants·hm-2 and HD, 97500 plants·hm-2) under mixed-cropping (M, 1:1, 2:2) and monoculture of Zhengdan958 (ZD) and Denghai605 (DH). The results showed that with the increases of planting density, grain yield, 13C-photosynthate allocation to grain, dry matter accumulation, and leaf area index (LAI) increased, but the chlorophyll content and net photosynthetic rate decreased. No significant difference was observed between the monoculture and mixed-cropping at the density of 67500 plants·hm-2. However, at 97500 plants·hm-2, LAI, chlorophyll content, net photosynthetic rate and dry matter accumulation in mixed-cropping were higher than that in monoculture. Mixed-cropping promoted the transport of dry matter from the vegetative organs such as stem to the grain and the distribution of 13C-photosynthates to grain. Grain yield of summer maize significantly increased in mixed-cropping due to the increase of 1000-grain mass. Under high plant density, the mixed-cropping could enlarge photosynthetic area, maintain higher net photosynthetic rate, increase dry matter accumulation, improve the distribution of dry matter, promote the distribution of 13C-photosynthates to grains and thus increase the grain yield. Our results indicated that mixed-cropping could significantly increase the yield of close planting summer maize in Huang-Huai-Hai Plain.

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  • Authors: Hairu Jin; Jian Zhuge; Huiying Fang;

    Candida glycerinogenes is an aerobe which does not depend on sulphite for production of glycerol. With a sufficient O2 supply, up to 130 g glycerol l(-1) was produced with 2.6 g acetic acid l(-1) as by-product. However, with an insufficient O2 supply--with higher volumes of medium or at higher corn steep liquid concentrations--the glycerol concentration was lower because the by-products, ethanol, pyruvate and lactic acid, were produced in greater amounts, up to 45 g l(-1), 4.3 g l(-1), 1.6 g l(-1), respectively, whereas, less acetic acid (0.6 g l(-1)) was produced. In addition, ethanol decreased to 0.4 g l(-1) and the glycerol yield improved from 34 to 50% (w/w) by adding 50 g sulphite l(-1), nevertheless, acetic acid increased to 7.8 g l(-1).

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  • Authors: Kai Ning; Pei-Xin Zhang; Zhen-Jing Yang; Xian-Zhe Dong; +2 Authors

    The Quaternary sediment in the Ningbo Coastal Plain was the deposit due to sea-land interaction, which recorded information of past climate changes. The region is therefore an ideal area to study paleoclimate changes and sedimentary characteristics. We determined the stratigraphic division and paleoenvironmental evolution based on 14C and paleomagnetic dating, along with detailed analyses of lithology, pollen assemblage, foraminifera and ostracodes assemblage, and grain size of sediment in core Z02 located in the southeastern Ningbo Coastal Plain. The results showed that the boundary between the Holocene and Upper Pleistocene in the core Z02 record was at 30.5 m, the boundary between the Upper and Middle Pleistocene was at 82.65 m, and the boundary between the Quaternary and Lower Cretaceous was at 90 m. The Middle Pleistocene section of the core contained few sediments, while the Lower Pleistocene section was completely missed. During the late Pleistocene, the hydrodynamic conditions experienced energy levels of medium to medium low to medium, and sedimentary facies changed from alluvial lake to overbank to river to lake to alluvial lake to lake to overbank. During the Holocene, the hydrodynamic changes experienced energy levels of medium low to low to medium, and the sedimentary facies changed from shoreland to shallow sea to shoreland lake. The Ningbo Coastal Plain had experienced tectonic uplift, weathering and erosion stage in the Early and Middle Pleistocene, from warm and humid to dry in the Late Pleistocene, and from warm and humid to dry and cool in the Holocene, as revealed by the core Z02 record. This study provided useful information in investigating past environmental changes in the subtropical coastal region of eastern China.

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    Authors: Cai, Ruohong; Yu, Danlin; Oppenheimer, Michael; Cai, Ruohong; +2 Authors

    Researchers have extensively studied crop yield response to weather variations, while only a limited number of studies have attempted to identify spatial heterogeneity in this relationship. We explore spatial heterogeneity in corn yield response to weather by combining geographically weighted regression and panel regression. We find that temperature tends to have negative effects on U.S. corn yields in warmer regions and positive effects in cooler regions, with spatial heterogeneity at a fine scale. The spatial pattern of precipitation effects is more complicated. A further analysis shows that precipitation effects are sensitive to the existence of irrigation systems.

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    https://dx.doi.org/10.22004/ag...
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    Authors: Vitalina Babenko; Miroshnichenko Tetyana; Dmytro Zherlitsyn; Olena Dovgal; +2 Authors

    The processes of transformation of the energy space, namely the impact of alternative energy resources on it, are characterized by changes in the national economy in general and in the energy market in particular. The results of the analysis confirmed the significant dependence of electricity production indicators on renewable sources and such factors as GDP, CO2 emissions, total electricity production, which requires improvement of organizational and economic bases for policy development of state support for renewable energy technologies in countries with exogenous factors. The interdependence between electricity production from renewable sources and economic indicators in Ukrainian-Chilean relations using macroeconomic multifactor analysis based on the correlation method allowed to identify the most influential factors.

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    Authors: Tong, Shi Lu; Olsen, Jorn; Kinney, Patrick L.;
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    Résumé. L'émission biogénique d'oxyde nitrique (NO) du sol a un impact important sur un certain nombre de questions environnementales, telles que la production d'ozone troposphérique, le cycle du radical hydroxyle (OH) et la production de NO. Dans cette étude, nous avons collecté les sols de quatre types de parcelles de végétation différents (pan, prairie annuelle, prairie vivace et brousse empiétée) dans un écosystème de savane aride du Kalahari (Botswana). Une technique d'incubation en laboratoire a été utilisée pour déterminer le flux net potentiel de NO des sols en fonction de l'humidité du sol et de la température du sol. Les émissions potentielles nettes de NO ont été augmentées pour l'année 2006 et une région (185 km×185 km) du sud du Kalahari. Pour cela, nous avons utilisé (a) les émissions potentielles nettes de NO mesurées en laboratoire, (b) la distribution des parcelles de végétation obtenue à partir des mesures NDVI de Landsat, (c) les teneurs en humidité du sol estimées obtenues à partir des mesures ENVISAT ASAR et (d) la température de surface du sol estimée à l'aide des mesures de température de surface MODIS MOD11A2 sur 8 jours. Les différences dans les flux de NO potentiels nets entre les parcelles de végétation se produisent et vont de 0,27 ng m−2 s−1 dans les parcelles de Pan à 2,95 ng m−2 s−1 dans les parcelles de prairie vivace. La mise à l'échelle des flux de NO potentiels nets avec les données satellitaires sur l'humidité et la température du sol a donné des flux de NO allant jusqu'à 323 g ha−1 mois−1, où les flux de NO les plus élevés se sont produits dans les parcelles de prairies vivaces et les plus bas dans les parcelles de Pan. Une tendance saisonnière marquée a été observée où les flux les plus élevés se sont produits pendant les mois d'été austral (janvier et février) tandis que les flux minimums se sont produits pendant les mois d'hiver austral (juin et juillet), et étaient inférieurs à 1,8 g ha−1 mois−1. Au cours de l'année, les émissions moyennes de NO pour la région mise à l'échelle étaient de 0,54 kg ha−1 an−1, ce qui représente une perte allant jusqu'à 7,4 % de l'apport d'azote (N) dans la région par les dépôts atmosphériques et la fixation biologique de l'azote. L'émission biogénique de NO du sol est donc un mécanisme important de perte d'azote de cet écosystème de savane aride et a le potentiel de jouer un rôle important dans la production d'ozone troposphérique et le cycle OH. Resumen. La emisión biogénica de óxido nítrico (NO) del suelo tiene un impacto importante en una serie de cuestiones ambientales, como la producción de ozono troposférico, el ciclo del radical hidroxilo (OH) y la producción de NO. En este estudio recolectamos suelos de cuatro tipos diferentes de parches de vegetación (Pan, Annual Grassland, Perennial Grassland y Bush Encroached) en un ecosistema de sabana árida en el Kalahari (Botswana). Se utilizó una técnica de incubación de laboratorio para determinar el flujo de NO potencial neto de los suelos en función de la humedad del suelo y la temperatura del suelo. Las emisiones netas potenciales de NO se aumentaron para el año 2006 y una región (185 km×185 km) del Kalahari meridional. Para ello, utilizamos (a) las emisiones potenciales netas de NO medidas en el laboratorio, (b) la distribución de parches de vegetación obtenida a partir de las mediciones de Landsat NDVI, (c) los contenidos estimados de humedad del suelo obtenidos a partir de las mediciones de ENVISAT asar y (d) la temperatura de la superficie del suelo estimada utilizando las mediciones de temperatura de la superficie terrestre MODIS MOD11A2 de 8 días. Se producen diferencias en el potencial neto de flujos de NO entre parches de vegetación y van desde 0.27 ng m−2 s−1 en los parches de Pan hasta 2.95 ng m−2 s−1 en los parches de pastizales perennes. La ampliación de los flujos de NO potenciales netos con los datos de humedad y temperatura del suelo obtenidos por satélite dio NO flujos de hasta 323 g ha−1 mes−1, donde los mayores flujos de NO aumentados ocurrieron en los parches de pastizales perennes y los más bajos en los parches de pan. Se observó un patrón estacional marcado donde los flujos más altos ocurrieron en los meses de verano australes (enero y febrero) mientras que los flujos mínimos ocurrieron en los meses de invierno australes (junio y julio), y fueron menores a 1.8 g ha−1 mes−1. A lo largo del año, la emisión media de NO para la región aumentada fue de 0,54 kg ha−1 año−1, lo que representa una pérdida de hasta el 7,4% de la entrada de nitrógeno (N) a la región a través de la deposición atmosférica y la fijación biológica de N. La emisión biogénica de NO del suelo es, por lo tanto, un mecanismo importante de pérdida de N de este ecosistema de sabana árida y tiene el potencial de desempeñar un papel importante en la producción de ozono troposférico y el ciclo de OH. Abstract. The biogenic emission of nitric oxide (NO) from the soil has an important impact on a number of environmental issues, such as the production of tropospheric ozone, the cycle of the hydroxyl radical (OH) and the production of NO. In this study we collected soils from four differing vegetation patch types (Pan, Annual Grassland, Perennial Grassland and Bush Encroached) in an arid savanna ecosystem in the Kalahari (Botswana). A laboratory incubation technique was used to determine the net potential NO flux from the soils as a function of the soil moisture and the soil temperature. The net potential NO emissions were up-scaled for the year 2006 and a region (185 km×185 km) of the southern Kalahari. For that we used (a) the net potential NO emissions measured in the laboratory, (b) the vegetation patch distribution obtained from Landsat NDVI measurements, (c) estimated soil moisture contents obtained from ENVISAT ASAR measurements and (d) the soil surface temperature estimated using MODIS MOD11A2 8 day land surface temperature measurements. Differences in the net potential NO fluxes between vegetation patches occur and range from 0.27 ng m−2 s−1 in the Pan patches to 2.95 ng m−2 s−1 in the Perennial Grassland patches. Up-scaling the net potential NO fluxes with the satellite derived soil moisture and temperature data gave NO fluxes of up to 323 g ha−1 month−1, where the highest up-scaled NO fluxes occurred in the Perennial Grassland patches, and the lowest in the Pan patches. A marked seasonal pattern was observed where the highest fluxes occurred in the austral summer months (January and February) while the minimum fluxes occurred in the austral winter months (June and July), and were less than 1.8 g ha−1 month−1. Over the course of the year the mean NO emission for the up-scaled region was 0.54 kg ha−1 yr−1, which accounts for a loss of up to 7.4% of the nitrogen (N) input to the region through atmospheric deposition and biological N fixation. The biogenic emission of NO from the soil is therefore an important mechanism of N loss from this arid savanna ecosystem and has the potential to play an important role in the production of tropospheric ozone and the OH cycle. الخلاصة. للانبعاث الحيوي لأكسيد النيتريك (NO) من التربة تأثير مهم على عدد من القضايا البيئية، مثل إنتاج الأوزون التروبوسفيري، ودورة جذر الهيدروكسيل (OH) وإنتاج NO. في هذه الدراسة جمعنا التربة من أربعة أنواع مختلفة من الرقع النباتية (عموم، المراعي السنوية، المراعي المعمرة وبوش التعدي) في النظام البيئي السافانا القاحلة في كالاهاري (بوتسوانا). تم استخدام تقنية الحضانة المختبرية لتحديد صافي تدفق NO المحتمل من التربة كدالة لرطوبة التربة ودرجة حرارة التربة. تم رفع صافي انبعاثات NO المحتملة لعام 2006 ومنطقة (185 كم×185 كم) من جنوب كالاهاري. لذلك استخدمنا (أ) صافي انبعاثات NO المحتملة المقاسة في المختبر، (ب) توزيع رقعة الغطاء النباتي الذي تم الحصول عليه من قياسات Landsat NDVI، (ج) محتويات رطوبة التربة المقدرة التي تم الحصول عليها من قياسات ENVISAT ASAR و (د) درجة حرارة سطح التربة المقدرة باستخدام قياسات درجة حرارة سطح الأرض MODIS MOD11A2 لمدة 8 أيام. تحدث اختلافات في صافي التدفقات المحتملة بين بقع الغطاء النباتي وتتراوح من 0.27 نانوغرام م -2 ثانية-1 في بقع المقلاة إلى 2.95 نانوغرام م-2 ثانية-1 في بقع المراعي المعمرة. لم ينتج عن زيادة صافي تدفقات NO المحتملة مع بيانات رطوبة التربة ودرجة الحرارة المستمدة من القمر الصناعي أي تدفقات تصل إلى 323 جم هكتار-1 شهر-1، حيث حدثت أعلى تدفقات NO على نطاق واسع في بقع المراعي المعمرة، وأدناها في بقع المقلاة. لوحظ نمط موسمي ملحوظ حيث حدثت أعلى التدفقات في أشهر الصيف الأسترالية (يناير وفبراير) بينما حدث الحد الأدنى من التدفقات في أشهر الشتاء الأسترالية (يونيو ويوليو)، وكانت أقل من 1.8 جم هكتار-1 شهر-1. على مدار العام، كان متوسط انبعاثات NO للمنطقة الصاعدة 0.54 كجم هكتار-1 سنة-1، وهو ما يمثل خسارة تصل إلى 7.4 ٪ من مدخلات النيتروجين (N) إلى المنطقة من خلال الترسب في الغلاف الجوي والتثبيت البيولوجي لـ N. وبالتالي، فإن الانبعاثات الحيوية من NO من التربة هي آلية مهمة لفقدان N من هذا النظام البيئي للسافانا القاحلة ولديها القدرة على لعب دور مهم في إنتاج الأوزون التروبوسفيري ودورة OH.

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  • Authors: Ming-Ming Li; Gang Li;

    Based on 98 Chinese pine (Pinus tabuliformis) tree-ring width data, normalized diffe-rence vegetation index (NDVI) data and land cover data in the Helan Mountains, we used VS-oscilloscope model to simulate the radial growth process of Chinese pine and to examine the relationship between vegetation canopy phenology and tree cambium phenology. Results showed that the end of season (EOS) of the vegetation canopy was significantly correlated with the EOS of the Chinese pine cambium. Such correlation was stronger than that between grassland and cambium. The start of season (SOS) and EOS of Chinese pine were related to the averaged minimum temperature in May-June and August-September, respectively. When the average minimum temperature in May-June increased by 1 ℃, SOS would be advanced by 4.3 days. The averaged minimum temperature in August-September increased by 1 ℃, EOS would be delayed by 2.6 days. The correlation between the phenology of vegetation canopy and the phenology of the cambium in Chinese pine differed among vegetation types. Simulating tree growth dynamics only through a tree-ring physiology model might lead to biased results. Using remote sensing monitoring data to combine canopy development and cambium growth would help to more accurately understand tree growth dynamics.

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  • Authors: Rui Li; Qi-Jie Yang;

    Alsophila spinulosa is a rare and endangered relict fern species. With the Maxent model, we predicted the global potential suitable habitat and its future changes for A. spinulosa. We evaluated the accuracy of our prediction based on the receiver operating characteristic curve (ROC), in order to provide reference for the protection, detection and cultivation of its resources. The results showed that most potential suitable habitat for A. spinulosa would be in Asia and few in North Ame-rica, Central America, Madagascar, La Réunion, Mauritius, Seychelles, New Zealand, New Caledonia and Fiji. The global potential suitable habitat for A. spinulosa under current climate conditions encompassed 357.1×104 km2, with Asia accounting for 88.4% and China for 49.5% of the total. The highly suitable habitat for A. spinulosa in China would be mainly in Yunnan-Guizhou Plateau, Sichuan Basin, south of the Nanling Mountains and Taiwan Island. The critical factors driving the distribution of A. spinulosa would be the precipitation of warmest quarter, July average precipita-tion, temperature seasonality and mean diurnal range. Under the SSP1_2.6 climate scenario, the global potential suitable habitat for A. spinulosa would decrease by 7.8% from 2041 to 2060, and increase by 3.2% from 2081 to 2100. Under the SSP2_4.5 climate scenario, it would increase by 2.9% from 2041 to 2060 and by 7.2% from 2081 to 2100. Under the SSP5_8.5 climate scenario, it would increase by 3.3% from 2041 to 2060 and by 5.3% from 2081 to 2100.

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