ERE
Energy, Resources and the Environment

Energy, Resources and the Environment

The Pore Space Scramble

by Alexandra Gormallya and Michelle Benthamb
aLancaster Environment Centre, Lancaster University, Lancaster, LA1 4YQ, UK; bBritish Geological Survey, Keyworth, Nottingham, NG12 5GG, UK

The underground is being used more to help us meet some of the challenges facing humans from tackling climate change, waste disposal to ensuring energy security. The notion of ‘pore space’ and its commodification, has gained much momentum over the last few years in policy circles, industry and the natural (geo)sciences alike. However ‘pore space’ and the use of the underground is now also being discussed within the social sciences too. Human geographers in particular are starting to critically discuss some of the ways in which society uses, perceives and interacts with the subsurface in the past, present, and different ways of how this might happen in the future. Through this examination, social scientists are beginning to interact with geoscientists. This has led to a collaborative engagement between human geographers in the Lancaster Environment Centre, with geoscientists at the British Geological Survey. Through this collaboration the notion of The Pore Space Scramble was born.

So, what is pore space and why might there be such a scramble for its use? Pore spaces are voids between rock grains that contain liquid or gas. The connection of pores then form pathways in which water, oil or gas can move. The interest in pore space therefore, is of interest due to its potential to store materials such as heat, gas or water. Uses of the pore space form a complex system so to simplify this we frame our discussion around the use of pore space for the long-term storage of CO2 as a result of Carbon Capture and Storage (CCS). CCS is a suggested route to decarbonising the power and industrial sectors.

Going down in scale: from the outcrop to the pore space (by the British Geological Survey)

Going down in scale: from the outcrop to the pore space (by the British Geological Survey)

There is strong political will behind CCS both at the European level and in the UK itself [1], the UK setting out a 3 phase road map to commercialise CCS going forward. Given this political drive, it is not only necessary to understand the technical capabilities and practical ability to take this technology forward it also raises many questions around society and governance of such a system into the future. For example, who has precedence over this space and how does it compete with other energy infrastructure on both the surface and subsurface (eg. oil & gas industry, windfarms)? What are the legal and regulatory standpoints of this space i.e. who owns the pore space and therefore legally be able to utilise its use? What are the long-term stewardship plans of this space (eg. 10, 100, 1000 years), how does this effect liability and how might the precedence of such industries change over time? Ultimately, how do we ethically and justly govern such a space both presently and when projected into the future?

Demands on the subsurface (by the British Geological Survey)

Demands on the (sub)surface (by the British Geological Survey)

We do not currently have answers for these questions but are initiating and undertaking research in this area as well as highlighting the need for policymakers, scientists, academic and publics to negotiate the challenges the subsurface will face going forward.

Reference:

  1. DECC (2012). CCS Roadmap: Supporting deployment of Carbon Capture and Storage in the UK < www.gov.uk/government/uploads/system/uploads/attachment_data/file/48317/4899-the-ccs-roadmap.pdf > Accessed: 10/06/2015.

Words on Wednesday: Do Himalayan treelines respond to recent climate change? An evaluation of sensitivity indicators

Words on Wednesday aims at promoting interesting/fun/exciting publications on topics related to Energy, Resources and the Environment. If you would like to be featured on WoW, please send us a link of the paper, or your own post, at ERE.Matters@gmail.com.

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Schickhoff, U., Bobrowski, M., Böhner, J., Bürzle, B., Chaudhary, R. P., Gerlitz, L., Heyken, H., Lange, J., Müller, M., Scholten, T., Schwab, N., and Wedegärtner, R., 2015. Do Himalayan treelines respond to recent climate change? An evaluation of sensitivity indicators, Earth Syst. Dynam., 6, 245-265.

Abstract:

Climate warming is expected to induce treelines to advance to higher elevations. Empirical studies in diverse mountain ranges, however, give evidence of both advancing alpine treelines and rather insignificant responses. The inconsistency of findings suggests distinct differences in the sensitivity of global treelines to recent climate change. It is still unclear where Himalayan treeline ecotones are located along the response gradient from rapid dynamics to apparently complete inertia. This paper reviews the current state of knowledge regarding sensitivity and response of Himalayan treelines to climate warming, based on extensive field observations, published results in the widely scattered literature, and novel data from ongoing research of the present authors.

Anthropogenic treeline in Manang, Nepal, showing an abrupt transition to alpine grazing lands (Schickhoff, 24 September 2013).

Anthropogenic treeline in Manang, Nepal, showing an abrupt transition to alpine grazing lands (Schickhoff, 24 September 2013).

Several sensitivity indicators such as treeline type, treeline form, seed-based regeneration, and growth patterns are evaluated. Since most Himalayan treelines are anthropogenically depressed, observed advances are largely the result of land use change. Near-natural treelines are usually krummholz treelines, which are relatively unresponsive to climate change. Nevertheless, intense recruitment of treeline trees suggests a great potential for future treeline advance. Competitive abilities of seedlings within krummholz thickets and dwarf scrub heaths will be a major source of variation in treeline dynamics. Tree growth–climate relationships show mature treeline trees to be responsive to temperature change, in particular in winter and pre-monsoon seasons. High pre-monsoon temperature trends will most likely drive tree growth performance in the western and central Himalaya. Ecological niche modelling suggests that bioclimatic conditions for a range expansion of treeline trees will be created during coming decades.

Climatic treeline (3900–4000 m) on a north-facing slope in Rolwaling, Nepal (Schwab, 18 September 2014).

Climatic treeline (3900–4000 m) on a north-facing slope in Rolwaling, Nepal (Schwab, 18 September 2014).

Funding opportunity for Early Career Researchers to attend GSA Baltimore

The Heritage Stone Task Group in southern Europe is a Task Group within the IUGS. In March, HSTG  had a proposal accepted as Project 637 of the International Geoscience Programme (IGCP 637). With this acceptance, IGCP 637 offered $US6,000 in 2015 to support conference participation.

HSTG has decided that this funding should be used in 2015 to support attendance to our session in the GSA Baltimore conference. Amounts not exceeding $US2000 will likely be available. We have been asked by the IGCP Secretariat to give preference to supporting scientists from developing countries or who are young or women scientists. Recipients will also be expected to make a conference presentation in our session, related to natural stones, architectonic heritage and related issues.

Early Career researchers who are interested should send a message showing interest and a short cv, with a potential title for the contribution in the HSTG session, to the HSTG secretary general Barry Cooper: Barry.Cooper@unisa.edu.au

Applicatons will be received up to 30 June 2015.

Please contact Dr Lola Pereira for further information (mdp@usal.es)

Down by the River: Environmental Impact of Energy Generation Along the Colorado River

In our hunt for energy, we turn in many directions, especially those that will affect the environment to a lesser extent than the conventional fossil fuels. Though renewable energy is a sustainable form of energy production – it is after all infinite – it does not always mean that this form of energy production is without impact.

In 1963 the Glen Canyon Dam was built across the Colorado River, running through the Grand Canyon. Doing so created Lake Powell and helped in the generation of hydroelectric power. By 1974, researchers discovered the impact the dam had further downstream along the Colorado River, with shrinking sandbars as they no longer were replenished by sediment trapped in Lake Powell, behind the dam. Since then, scientists have been trying to get insight into the possibility of controlled flooding of the river to maintaining, or growing, the number of sandbars in the Colorado River. A new High Flow Experimental Release (HFE) Protocol could be the solution. However, care needs to be taken to protect both the downstream eco-system, as well as ensuring sufficient power generation by the dam.

Read more in this week’s EOS article 🙂

Colorado Horseshoe Bend (by Ioannis Daglis, taken from ImagGeo)

Colorado Horseshoe Bend (by Ioannis Daglis, taken from ImagGeo)