The time and place for political ecology: An introduction to the articles honoring the life-work of Piers Blaikie

Political ecology (PE) is experiencing a renaissance and embrace similar to that of Geography itself. Just as there is a rediscovery of the importance of place and thus Geography, Geographers and others are discovering that this critical approach to the human-environment dialectic provides unique theoretical, methodological, and practical insights for unravelling the complexities of this contentious nexus. The host of new volumes that introduce students and the larger academic community to PE each emphasize different theoretical and thematic confluences. This volume is organized around the life-long work and intellectual history of a leading political ecologist, Piers Blaikie, and as such it is both a tribute to that work, and an alternative means to discover what PE is today. Piers Blaikie’s life-work also encompasses research and writing on natural disasters and risk, development policy and practice, international environmental policy, conservation and biodiversity, AIDS in Africa, livelihoods, and books on India and Nepal. By assessing Blaikie’s long and productive career, from pioneering foundational texts, through transdisciplinary exchanges in the fields of Geography, Development Studies, and policy, to constructive and critical engagement with the post-modern turn, and questions of epistemology and methodology, the contributions to this themed issue provide a diverse yet coherent set of insights. The three sessions of the Association of American Geographers (AAG) Conference in Denver in 2005 and group of articles that emerged from them to form this collection serve to clarify the major convergences and dissonances in the field and its ongoing vitality. In Piers Blaikie’s case, as a central actor in both the theory and practice of PE, a collection based upon a critical overview of his contributions to PE provides a new window into seeing and understanding the past, present, and future of the field.     

High-pressure behavior of natural single-crystal epidote and clinozoisite up to 40 GPa

The comparative compressibility and high-pressure stability of a natural epidote (0.79 Fe-total per formula unit, Fe_tot pfu) and clinozoisite (0.40 Fe_tot pfu) were investigated by single-crystal X-ray diffraction and Raman spectroscopy. The lattice parameters of both phases exhibit continuous compression behavior up to 30 GPa without evidence of phase transformation. Pressure–volume data for both phases were fitted to a third-order Birch–Murnaghan equation of state with V ₀ = 461.1(1) ų, K ₀ = 115(2) GPa, and \(K_{0}^{'}\) = 3.7(2) for epidote and V ₀ = 457.8(1) ų, K ₀ = 142(3) GPa, and \(K_{0}^{'}\) = 5.2(4) for clinozoisite. In both epidote and clinozoisite, the b-axis is the stiffest direction, and the ratios of axial compressibility are 1.19:1.00:1.15 for epidote and 1.82:1.00:1.19 for clinozoisite. Whereas the compressibility of the a-axis is nearly the same for both phases, the b- and c-axes of the epidote are about 1.5 times more compressible than in clinozoisite, consistent with epidote having a lower bulk modulus. Raman spectra collected up to 40.4 GPa also show no indication of phase transformation and were used to obtain mode Grüneisen parameters (γ _i) for Si–O vibrations, which were found to be 0.5–0.8, typical for hydrous silicate minerals. The average pressure coefficient of Raman frequency shifts for M–O modes in epidote, 2.61(6) cm^?1/GPa, is larger than found for clinozoisite, 2.40(6) cm^?1/GPa, mainly due to the different compressibility of FeO₆ and AlO₆ octahedra in M3 sites. Epidote and clinozoisite contain about 2 wt% H₂O are thus potentially important carriers of water in subducted slabs.     

The analysis of using satellite soil moisture observations for flood detection,evaluating over the Thailand’s Great Flood of 2011

Natural Hazards - A flood monitoring and warning system provides critical information that can protect property and save lives. A basin-scale flood monitoring system requires an effective...     

Hierarchical livelihood outcomes among co-managed fisheries

Collaborative management arrangements are increasingly being used in fisheries, yet critical questions remain about the conditions under which these are most successful. Here, we conduct one of the first comprehensive tests of Elinor Ostrom's diagnostic framework for analyzing social–ecological systems to examine how 16 socioeconomic and institutional conditions are related the livelihood outcomes in 42 co-management arrangements in five countries across the Indo-Pacific. We combine recent developments in both theory and modeling to address three key challenges among comparative studies of social–ecological systems: the presence of a large number of explanatory mechanisms, variables operating at multiple scales, and the potential for interactions among socio-economic and institutional factors. We find that resource users were more likely to perceive benefits from co-management when they are more involved in decisions, were aware that humans are causal agents of change in marine systems, were wealthier, were not migrants, were in villages with smaller populations and older co-management arrangements, and had clearly established boundaries. Critically, we quantify a number of key interactions between: wealth, dependence on marine resources, involvement in decision-making, and population size that have strong implications for co-management success in terms of livelihood benefits. This study demonstrates that context plays a critical but identifiable role in co-management success.     

Multi-spectral imaging of vegetation for detecting CO<Subscript>2</Subscript> leaking from underground

Practical geologic CO₂ sequestration will require long-term monitoring for detection of possible leakage back into the atmosphere. One potential monitoring method is multi-spectral imaging of vegetation reflectance to detect leakage through CO₂-induced plant stress. A multi-spectral imaging system was used to simultaneously record green, red, and near-infrared (NIR) images with a real-time reflectance calibration from a 3-m tall platform, viewing vegetation near shallow subsurface CO₂ releases during summers 2007 and 2008 at the Zero Emissions Research and Technology field site in Bozeman, Montana. Regression analysis of the band reflectances and the Normalized Difference Vegetation Index with time shows significant correlation with distance from the CO₂ well, indicating the viability of this method to monitor for CO₂ leakage. The 2007 data show rapid plant vigor degradation at high CO₂ levels next to the well and slight nourishment at lower, but above-background CO₂ concentrations. Results from the second year also show that the stress response of vegetation is strongly linked to the CO₂ sink–source relationship and vegetation density. The data also show short-term effects of rain and hail. The real-time calibrated imaging system successfully obtained data in an autonomous mode during all sky and daytime illumination conditions.