Nuclear power is low-carbon and green energy. It presently provides about 10% of the world's electricity and 20% of the UK's electricity, contributing enormously to global Net Zero emissions. Nuclear power will continue to play an important role in the global transition to a low carbon economy. However, one major disadvantage of nuclear power is that its generation process produces radioactive waste that can remain hazardous for hundreds of thousands of years. Over the past more than 60 years' utilisation of nuclear power in the UK and worldwide, many radioactive wastes have accumulated, most of which are stored temporarily in storage near nuclear power plants. It is vital for us to deal with the waste to protect human health and the environment. A global consensus has been reached in this area, that is to isolate radioactive waste that is incompatible with surface disposal permanently in suitable underground rock formations (i.e., host rocks) by developing a geological disposal facility (GDF). As also set out in the 2014 White Paper, the UK Government is committed to implementing geological disposal, with work on developing this led by Radioactive Waste Management Ltd (RWM). Developing a GDF relies on a stable rock formation to ensure mechanical stability and barrier function of host rocks. It is therefore essential to understand factors that influence the integrity of rocks. This is challenging partially because of the complexity of rock fractures that are widespread in the Earth upper crust. Although rock mechanical behaviour has a long record of study, attempts to understand the role of fractures on rock deformation still has unresolved issues. For example, natural rock fractures are often dealt with crudely; almost all previous studies of this problem assume rock fractures to be continuous, with zero or very small cohesion that can be neglected. However, it is almost a ubiquitous feature that natural rock fractures in the subsurface are incipient and heterogeneous, with considerable tensile strength and cohesion. This is either due to secondary minerals having recrystallised, bonding fracture surfaces together, or due to rock bridges. This INFORM project will focus on mineral-filled fractures (i.e., veins) that are frequently seen in the subsurface but often ignored or less researched so far. The aim of INFORM is to increase confidence in the design, construction, and operation of GDFs, by developing a mechanics-based multi-scale framework to understand the influence of fracture heterogeneity on the integrity and deformation behaviour of rocks across scales. The framework will integrate imaging analysis, laboratory experiments, numerical modelling, and field observations, to (1) determine factors contributing to fracture heterogeneity across scales, (2) understand the shear and triaxial deformational behaviour of veined rocks considering natural fracture geometry and heterogeneity, and (3) develop a field-scale model for repository structures considering fracture heterogeneity. Unlike most previous studies, which have focused on the influence of mechanical fractures on rock behaviour, INFORM will for the first time investigate the influence of natural veins, and will consider and implement these observations in the modelling of veined rock behaviour applied to a GDF. INFORM will "inform" a wide range of audiences with new insights through correlating micro-scale observations and macro-scale deformation of heterogenous veined and fractured rocks. This will be possible with the strong support of our academic and industrial partners (RWM, UK; Jacobs, UK; Northeastern University, China; GFZ, Germany; Stanford University, USA) and the help of our well-designed outreach and publication plans. INFORM will lead to a more accurate and reliable examination of fracture heterogeneity, which will not only directly benefit GDF R&D, but also broader rock engineering applications (e.g., tunnelling, cavern construction).

This research proposal links to the International Ocean Discovery Program (IODP) Expedition 396 which will drill several scientific research boreholes along the offshore Norwegian continental margin. The Norwegian margin is one of the best studied examples of a passive rifted margin associated with voluminous magmatic activity. However, key scientific questions associated with the origins of magmatism and its impacts on global climate at this time remain. The objectives of the cruise cover a wide range of high impact scientific research areas including assessing the role of the Iceland plume on excess magmatism, understanding along axis variations in magmatism, determining the nature and depositional environment of volcanism, and assessing the role that magmatism played in driving global warming (Paleocene Eocene Thermal Maximum or PETM) at this time. A secondary goal of the expedition is to appraise the potential of permanent carbon capture and storage (CCS) in the volcanic sequences. This research project will address several of the EXP 396 objectives focusing on three specific areas of research. Objective 1: Understanding the interplay between magmatism and eruption environments during rifting. Volcanic cores will be used to appraise how volcanism and the environment of eruption changed in space and time during continental rifting. Detailed facies analyses of the volcanic sequences will be undertaken to reveal whether the eruptions occurred within subaerial, marginal, or subaqueous environments. Geophysical logging data will be used alongside core observations to build a comprehensive and integrated volcanological model for the borehole penetrated sequences. The geophysical volcanic model will then be used to calibrate extensive 3D seismic surveys in the area which in turn will enable mapping of volcanic facies over large parts of the margin. This aspect of the project will enable new understanding about how extrusive magmatism is linked to margin scale base-level changes which in turn will give new data for testing competing models for volcanic rifted margin evolution such as plume-pulsing versus plate tectonics. Objective 2: Appraising the carbon capture and storage (CCS) potential of break-up related volcanic sequences. Pilot studies on Iceland (Carbfix) and in Washington State, USA (Wallula), have demonstrated that CO2 reacts with basaltic rocks to form carbonate minerals, effectively permanently storing the CO2. Permanent storage clearly reduces the risk of leakage and has been demonstrated to occur over incredibly rapid timescales on the order of a few years. The huge volume of offshore break-up related volcanic sequences that will be tested during EXP. 396 could offer an alternative storage site for permanent storage of anthropogenic CO2. Volcanic sequences can have good reservoir properties, however, extensive weathering and alteration can also significantly diminish and clog up the pore structure. Within this study petrophysical analyses of volcanic cores will be performed to give important new constraints on the reservoir potential and sealing capacity of the Atlantic margin volcanic sequences. Objective 3: Understanding the temporal and spatial evolution of magma petrogenesis within the province and its potential role in driving the PETM. Geochemical analyses from the various volcanic sequences will be used to appraise whether elevated and/or fluctuating mantle temperatures led to excess magmatism in mid-Norway. Regional datasets will be compared to appraise how melting changed along the margin and whether these results resolve competing plume or plate tectonic models. Some sites will target hydrothermal vents associated with break-up related intrusions which caused massive emissions of Greenhouse gases. High resolution core-log-seismic appraisal coupled with isotopic dating of the ejecta layers will hopefully improve the age constraints on these processes in order to better appraise links to the PETM.

Volcanic eruptions are an ever-present hazard facing society both in terms of their immediate devastation, but also global disruption to flights, trade and economic development. While petrological insights into magmatic processes are possible following an eruption, as yet there exists no way to link present day volcano-monitoring techniques to an understanding of the magmatic plumbing system, and its effects on the duration, size and magnitude of the volcanic eruptions prior to and during volcanic crises. This proposal seeks to establish a multidisciplinary team of Earth scientists to attempt to link the geophysical observations of upper crustal stress state (compression, extension, transtension) with petrological inferences of magma storage conditions. Once established, this team will look to undertake some initial data collection of the time it takes for magma to rise and be erupted, at carefully selected target volcanoes which are known to be in different stress states. Longer-term, this new team of experts will look to use the initial data collected from this Global Partnerships Seedcorn Fund to establish a series of crustal stress-magmatism archetypes to be tested and applied at volcanic arcs worldwide. There is potential that in the future, timescales between unrest and eruption at poorly-monitored volcanoes could be better anticipated based on volcanism-stress archetypes coupled with remote observations of upper crustal stress states.

Nuclear power is low-carbon and green energy. It presently provides about 10% of the world's electricity and 20% of the UK's electricity, contributing enormously to global Net Zero emissions. Nuclear power will continue to play an important role in the global transition to a low carbon economy. However, one major disadvantage of nuclear power is that its generation process produces radioactive waste that can remain hazardous for hundreds of thousands of years. Over the past more than 60 years' utilisation of nuclear power in the UK and worldwide, many radioactive wastes have accumulated, most of which are stored temporarily in storage near nuclear power plants. It is vital for us to deal with the waste to protect human health and the environment. A global consensus has been reached in this area, that is to isolate radioactive waste that is incompatible with surface disposal permanently in suitable underground rock formations (i.e., host rocks) by developing a geological disposal facility (GDF). As also set out in the 2014 White Paper, the UK Government is committed to implementing geological disposal, with work on developing this led by Radioactive Waste Management Ltd (RWM). Developing a GDF relies on a stable rock formation to ensure mechanical stability and barrier function of host rocks. It is therefore essential to understand factors that influence the integrity of rocks. This is challenging partially because of the complexity of rock fractures that are widespread in the Earth upper crust. Although rock mechanical behaviour has a long record of study, attempts to understand the role of fractures on rock deformation still has unresolved issues. For example, natural rock fractures are often dealt with crudely; almost all previous studies of this problem assume rock fractures to be continuous, with zero or very small cohesion that can be neglected. However, it is almost a ubiquitous feature that natural rock fractures in the subsurface are incipient and heterogeneous, with considerable tensile strength and cohesion. This is either due to secondary minerals having recrystallised, bonding fracture surfaces together, or due to rock bridges. This INFORM project will focus on mineral-filled fractures (i.e., veins) that are frequently seen in the subsurface but often ignored or less researched so far. The aim of INFORM is to increase confidence in the design, construction, and operation of GDFs, by developing a mechanics-based multi-scale framework to understand the influence of fracture heterogeneity on the integrity and deformation behaviour of rocks across scales. The framework will integrate imaging analysis, laboratory experiments, numerical modelling, and field observations, to (1) determine factors contributing to fracture heterogeneity across scales, (2) understand the shear and triaxial deformational behaviour of veined rocks considering natural fracture geometry and heterogeneity, and (3) develop a field-scale model for repository structures considering fracture heterogeneity. Unlike most previous studies, which have focused on the influence of mechanical fractures on rock behaviour, INFORM will for the first time investigate the influence of natural veins, and will consider and implement these observations in the modelling of veined rock behaviour applied to a GDF. INFORM will "inform" a wide range of audiences with new insights through correlating micro-scale observations and macro-scale deformation of heterogenous veined and fractured rocks. This will be possible with the strong support of our academic and industrial partners (RWM, UK; Jacobs, UK; Northeastern University, China; GFZ, Germany; Stanford University, USA) and the help of our well-designed outreach and publication plans. INFORM will lead to a more accurate and reliable examination of fracture heterogeneity, which will not only directly benefit GDF R&D, but also broader rock engineering applications (e.g., tunnelling, cavern construction).

There is a recognised gap in the communication of information generated by climate scientists and evidence needed by policy makers, in part because influencing policy through research is complex and requires skills that might not be valued or common in research systems. The current situation of our Earth's system, together with the social movements for climate justice, urge a step change in how policy and scientists approach Climate Change. Through this fellowship, I will develop new routes for impact in palaeoclimatology and will lead a vital step change in my field of research. Annual to decadal climate predictions may offer important information to Climate Services and Environmental Agencies, which would help guide short- and medium-term climate change strategies. For example, a better knowledge of the frequency and magnitude of floods in the UK. Decadal climate predictions are skilful for surface temperature, but confidence in projections of atmospheric pattern and the associated ecosystem response are less robust. This is, in part, because the amplitude of the decadal climate response is difficult to verify by the available instrumental data (reanalyses), which only goes back a century or two, and the impact of superimposed low-frequency variability might not be well represented. One way to provide more information on the decadal climate response is to include high-temporal resolution palaeoclimate timeseries in reanalyses. So far, the availability of proxy data suitable for this purpose is limited by the nature of the data (qualitative vs quantitative), chronological constrains (dating uncertainty and time-resolution of the proxy records) and geographical location of the proxy records (i.e limited to specific climate regions as ice-cores and corals), hence the study of decadal climate variability in the past is still in its infancy. In order to make developments in this field, I will lead an international research team that integrates palaeoclimatologists and climate modellers. We will combine emerging methodological approaches in proxy developments, chronological constraints, statistical tools and data-model comparison to provide advanced information of past decadal climate variability in the North Atlantic-European region such as shifting atmospheric circulation and occurrence of extreme weather events; and we will develop emergent constraints based on past climate scenarios to be applied to decadal prediction systems. Beyond the scientific goals, the fellowship aims at a better integration of palaeo evidence into climate policy to create a step change in how long-term climate data are viewed and used by policy and stakeholders. We will create a network of policy advisers, policy makers and other end users willing to engage. A co-development model of research will be adopted to develop shared understanding to design the research outputs, and ensure the research contributes to the specific and current needs of the decision makers across various sectors. The ultimate challenge is to create a leading centre for Palaeo Evidence for Policy at Royal Holloway University of London to: (1) build a palaeo-climate service feeding policy makers with evidence to assist decision-making; (2) support palaeoclimatologists in the UK and overseas to make impact cases studies; (3) train the next generation of early career researchers in policy skills. The fellowship will also explore art-based methods for impact. In particular, creative writing to promote climate science literacy for young children.