From Militant Particularism to Anti‐neoliberalism? The Anti‐Enron Movement in India

Abstract: The memorandum of understanding between Enron and the Maharashtra State Electricity Board, signed on 20 June 1992, set in motion the Dabhol Power Project, the largest corporate‐led venture in Indian history. But even while the project was gaining official clearance, it attracted considerable local opposition on environmental and livelihood related grounds. Additionally, the fact that Enron was awarded the contract by the Congress Party led state government of Maharashtra, in the absence of procedural transparency and open bidding, entangled the project in deep controversy. This paper, based on fieldwork, examines opposition to the Dabhol Power Project. I particularly focus on the relevance of militant particularism, and the importance of counter‐hegemony of the working class and/or the subaltern counter‐public in the context of multi‐scaled manifestations of neoliberal power.      

BOOK REVIEWS

Book reviewed in this article: Palestinian Rights: Affirmation and Denial. Edited by Ibrahim Abu-Lughod A Mediterranean Society: The Jewish Community of the Arab World as Portrayed in the Documents of the Cairo Geniza , Volume 4: Daily Life. By S. D. Goitein The Arabic Book. By Johannes Pedersen The Early Islamic Conquests. By Fred McGraw Donner The Islamic Impact. Edited by Yvonne Yazbeck Haddad, Byron Haines and Ellison Findly Persian Miniature Painting: and its Influence on the art of Turkey and India [The British Library Collections]. By Norah M. Titley Essays in Islamic Art and Architecture [Islamic Art and Architecture, Vol. I]. Edited by Abbas Daneshvari Architecture and Community: Building in the Islamic World Today. [The Aga Khan Award for Architecture.] Edited by Renata Holod with Darl Rastorfer Islam and Ownership. By Seyyed Mahmood Taleqani Society and Economics in Islam: Writings and Declarations of Ayatullah Sayyid Mahmud Taleghani. Translated from the Persian by R. Campbell Equality, Efficiency, and Property Ownership in the Islamic Economic System. By Akhtar A. Awan. Lanham Crime and Corrections: An Al-Islamic Perspective. By Sidney R. Sharif The Qur'ān and Its Interpreters. Vol. I. By Mahmoud M. Ayoub 'Ulum al-Qur'ān: An Introduction to the Sciences of the Qur'ān. By Ahmad von Denffer Ibn Taymiyyah's Ethics—The Social Factor. By Victor E. Makari Shāh Wal?-Allāh And His Times. By Saiyid Athar Abbas Rizvi Islamic Theology and Philosophy: Studies in Honor of George F. Hourani. Edited by Michael E. Marmura Religion, My Own. The Literary Works of Naj?b Ma fūz. By Mattityahu Peled L'Orient dèchirè entre I'Est et L'Ouest (1955–1982). By Simon Jargy The Reflowering of Malaysian Islam: Modern Religious Radicals and Their Roots. By Judith Nagata Muslim Sects and Divisions. The section on Muslim sects in Kitāb al-Milal wa'I-Ni al by Mu ammad b. 'Abd al-Kar?m Shahrastān? (d. 1153) . By A. K. Kazi and J. G. Flynn Muslim Intellectual Responses to “New Order” Modernization in Indonesia. By Muhammad Kamal Hassan Social history of Timbuktu: the role of Muslim scholars and notables 1400–1900. By Elias N. Saad Religion and Politics in Muslim Society : Order and Conflict in Pakistan. By Akbar S. Ahmed Baba of Karo: A Woman of the Muslim Hausa. By Mary F. Smith     

Boron isotope geochemistry of Na‐bicarbonate,Na‐chloride,and Ca‐chloride waters from the Northern Apennine Foredeep basin: other pieces of the sedimentary basin puzzle

The boron stable isotope ratio δ¹¹B of 12 water samples representative of three chemical facies (fresh Na‐bicarbonate, brackish Na‐chloride, saline, and brine Ca‐chloride) has been analyzed. Interpretation of the δ¹¹B data, along with the chemical compositions, reveals that Na‐carbonate waters from the Northern Apennine are of meteoric origin, with boron contributions from clay desorption and mixing with seawater‐derived fluids of Na‐chloride or Ca‐chloride compositions. The comparison of our new results with the literature data on other sedimentary basins of Mediterranean, and worldwide, confirms the contribution of Na‐bicarbonate waters to the genesis of mud volcano fluids. The Na‐chloride sample of Salvarola (SAL), which may represent the end‐member of the mud volcanoes, and the Ca‐chloride brine water from Salsomaggiore (SM) indicate boron release from clays compatible with the diagenetic process. The empirical equation: relating boron concentration and the stable isotope composition of the fluids observed in this study and the literature is proposed to trace the effect of diagenesis in sedimentary basins. A geothermometer associated to the diagenetic equation is also proposed: The application of this equation to obtain reservoir temperatures from δ¹¹B compositions of waters should be carefully evaluated against the results obtained from other chemical and isotopic geothermometers from other basins around the world.     

Industrial District and the Multiplication of Labour: The Chinese Apparel Industry in Prato,Italy

Since the 1990s, the Chinese apparel industry in Prato has developed from a few stitching workshops into full‐fledged production networks. However, persistent disparity between the Chinese and Italian labor has triggered widespread social tensions. Drawing upon the recent literature of critical labor studies, this paper offers a different perspective to see the disparity in terms of the multiplication of labor across scales. The Chinese labor in Prato is made cheap and flexible by the proliferation of institutional and social borders, which were in turn inadvertently produced by Italian immigration policies, Chinese social norms, and local and regional economic conditions. In particular, the Chinese migrant workers have played an active role in producing social borders and in their own exploitation. Therefore, the labor polarization in Prato can hardly be solved by local institutional arrangements, and Italian trade unions have failed to organize the Chinese migrant labor in Prato.     

Effects of pore fluid flow and chemistry on compaction creep of calcite by pressure solution at 150°C

Uni‐axial compaction creep experiments were performed on crushed limestone and analytical grade calcite powders at 150°C, a pore fluid pressure of 20 MPa, and effective axial stresses of 30 and 40 MPa. Previous experiments have shown that compaction under these conditions is dominated by intergranular pressure solution (IPS). The aim of the present tests was to determine the inter‐relationship between pore fluid chemistry, compaction rate and the rate‐controlling process of IPS. Intermittent flow‐through runs conducted using CaCO₃ solution showed no effect on creep rate at low strains (<4–5%) but a major acceleration at high strains (5–10%). Measurements of the Ca concentration present in fluid samples revealed the build‐up of a high super‐saturation of CaCO₃ during compaction under zero flow conditions, especially at high strains. Active flow‐through led to a drop in Ca concentration, which corresponded with creep acceleration. Addition of NaCl to the pore fluid, at a concentration of 0.5 m , increased the creep rate of the analytical grade calcite samples roughly in proportion to the enhancement of calcite solubility. Addition of Mg²⁺ and to the pore fluid, in concentrations of 0.05 and 0.001 m, respectively, caused major retardation of compaction creep. Integrating our mechanical, flow‐through and chemical data points strongly to diffusion‐controlled IPS being the dominant deformation mechanism in the calcite‐water system under closed‐system (zero flow) conditions at low strains (<4–5%), giving way to precipitation control at higher strains. Our fluid composition data suggest that this transition is because of accumulation of impurities in the pore fluid. As Mg²⁺ and phosphate ions are common in natural pore fluids, it is likely that retarded precipitation will be the rate‐limiting step of IPS in carbonates in nature. To quantify diagenetic compaction and porosity‐permeability reduction rates by IPS in carbonates needs to account for this.     

MICRO‐RAMAN SPECTROSCOPY CHARACTERIZATION OF DELLA ROBBIA GLAZES*

Micro‐Raman spectroscopy and the laser‐induced transformation technique were used for systematic study of five coloured glazes on Saint John the Baptist (29 inch tondo), a majolica terracotta relief attributed to Luca Della Robbia and on permanent exhibit in The John and Mable Ringling Museum of Art. We suggest that ions in a lead silicate matrix, called ‘lead ultramarine’, could contribute to the famous Della Robbia blue colour, in addition to the effect of Co atoms as suggested previously by Pappalardo et al. (2004 ). The original yellow glaze contains lead(II) antimonate. The green is a mixture of the yellow and blue pigments, the brown contains hematite, and the white glaze contains tin dioxide as an opacifier. The use of lead oxide as a main fluxing agent is confirmed by laser‐induced micro‐crystallization.     

Diffusion and kinetic control of weathering layer development

The formation of porous weathering rinds (layers of chemical alteration) on the exterior of rocks is a consequence of dissolution and precipitation of minerals occurring at the mineral–fluid interface within the pores. The speed at which the developed rind advances is controlled by both kinetic reaction rates and the transport of reaction products away from the pore spaces into the outside fluid. We show, using both reaction‐diffusion theory and numerics, that under diffusion limitations, the weathering rate depends on the size and curvature of the sample. This leads to a relationship between rind thickness, δ, and age, t. As the rind thickens, the result in three dimensions differs substantially from the one‐dimensional result of . We describe the conditions under which the one‐dimensional and diffusion‐limited approximations apply and how they evolve as the rock weathers. Under chemical kinetic limitations, the rind advances at a constant rate, dδ/dt = v. We defend the application of a spherical approximation to irregular non‐spherical rocks and apply our results to field observations reported in the literature to show consistency with established methods. Finally, we argue that the variability in size, as well as in mineralogy, over ensembles of grains contributes to heterogeneous weathering rates. We demonstrate that this heterogeneity can contribute to the aging, or gradual decrease with time, of weathering rates previously observed in laboratory and field measurements.     

On the Performance of the Subtour Elimination Constraints Approach for the p‐Regions Problem: A Computational Study

The p‐regions is a mixed integer programming (MIP) model for the exhaustive clustering of a set of n geographic areas into p spatially contiguous regions while minimizing measures of intraregional heterogeneity. This is an NP‐hard problem that requires a constant research of strategies to increase the size of instances that can be solved using exact optimization techniques. In this article, we explore the benefits of an iterative process that begins by solving the relaxed version of the p‐regions that removes the constraints that guarantee the spatial contiguity of the regions. Then, additional constraints are incorporated iteratively to solve spatial discontinuities in the regions. In particular we explore the relationship between the level of spatial autocorrelation of the aggregation variable and the benefits obtained from this iterative process. The results show that high levels of spatial autocorrelation reduce computational times because the spatial patterns tend to create spatially contiguous regions. However, we found that the greatest benefits are obtained in two situations: (1) when ; and (2) when the parameter p is close to the number of clusters in the spatial pattern of the aggregation variable.     

The Periplus,Pliny and Arabia

Factual differences between the Periplus and Pliny about Roman trade with India reveal a time gap which indicates a date for the Periplus of circa 45 AD. In the light of this, a number of conclusions concerning Arabia in the 1st century AD can be drawn, in particular that awr Rūnī is not the site of Moscha, while the historical background in the Persian Gulf can be more readily understood. Points touched on concerning the sea routes to India and Italian mediaeval versions of Ptolemy's map of Arabia are discussed more fully in two appendices.     

Effect of salinity on mass and energy transport by hydrothermal fluids based on the physical and thermodynamic properties of H2O‐NaCl

Various thermodynamic properties of H₂O that are defined as pressure or temperature derivatives of some other variable, such as isothermal compressibility (β, pressure derivative of density), isobaric thermal expansion (α, temperature derivative of density), and specific isobaric heat capacity (c_f, temperature derivative of enthalpy), all show large magnitudes near the critical point, reflecting large variations in fluid density and specific enthalpy with small changes in temperature and pressure. As a result, mass (related to fluid density) and energy (related to fluid enthalpy) transport in this PT region are sensitive to changing PT conditions. Addition of NaCl to H₂O causes the region of anomalous behavior, here defined as the critical region, to migrate to higher temperatures and pressures. The critical region is defined as that region of PT space in which the dimensionless reduced susceptibility  ≥ 0.5. When NaCl is added to H₂O, the critical region migrates to higher temperature and pressure. However, the absolute magnitudes of thermodynamic properties that are defined as temperature and/or pressure derivatives (α, β, and c_f) all decrease with increasing salinity. Thus, the mass and energy transporting capacities of hydrothermal fluids in the critical region become less sensitive to changing PT conditions as the salinity increases. For example, quartz solubility can be described as a function of fluid density, and because density becomes less sensitive to changing PT conditions as salinity increases, quartz solubility also becomes less sensitive to changing PT conditions as fluid salinity increases. Similarly, fluxibility describes the ability of a fluid to transport heat by buoyancy‐driven convection, and fluxibility decreases with increasing salinity. Results of this study show that the mass and energy transport capacity of fluids in the Earth's crust are maximized in the critical region and that the sensitivity to changing PT conditions decreases with increasing salinity.     

Grain‐scale permeabilities of faceted polycrystalline aggregates

Porous synthetic quartzites and amphibolites, each with faceted pore walls, were synthesized and evaluated to examine the permeability of pore networks similar to those of the lower crust and mantle. Quartzite with a fluid in equilibrium with an Mg–clinopyroxene contained connected networks of pores with a dihedral angle of 30° bounded by walls that were 10–50% faceted. The relationship of their permeability (k) to porosity (φ) is approximated by the previously determined relationship for relatively nonfaceted synthetic quartzite Amphibolite with an HF fluid contained fluorotremolite and a connected network of pores bounded by walls exhibiting 78–90% faceting. These materials showed much lower k for a given φ, with an apparent permeability threshold at φ_c = 0.04. A curve fit to these data yields The results suggest that moderate faceting has little effect on the transmission of fluids through rocks, but extensive faceting significantly alters permeability. This difference is most likely produced through isolation of the fluid to the grain corners at low φ with extensive faceting. Rocks with pores that tend toward faceting may impede the flow of fluids and melt.     

Opportunities and constraints for intensive agriculture in the Hawaiian archipelago prior to European contact

Intensive agricultural systems interact strongly and reciprocally with features of the lands they occupy, and with features of the societies that they support. We modeled the distribution of two forms of pre-European contact intensive agriculture – irrigated pondfields and rain-fed dryland systems – across the Hawaiian archipelago using a GIS approach based on climate, hydrology, topography, substrate age, and soil fertility. Model results closely match the archaeological evidence in defined locations. On a broader scale, we calculate that the youngest island, Hawai'i, could have supported 572 km² of intensive agriculture, 97% as rain-fed dryland field systems, while Kaua'i, the oldest island, could have supported 58 km², all as irrigated wetland systems. Irrigated systems have higher, more reliable yields and lower labor requirements than rain-fed dryland systems, so the total potential yield from Kaua'i (49k metric tons) was almost half that of Hawai'i (97k metric tons), although Kaua'i systems required only 0.05 of the agricultural labor (8400 workers, versus 165,000 on Hawai'i) to produce the crops. We conclude that environmental constraints to intensive agriculture across the archipelago created asymmetric production efficiencies, and therefore varying potentials for agricultural surplus. The implications both for the emergence of complex sociopolitical formations and for anthropogenic transformation of Hawaiian ecosystems are substantial.     

Zur Gestalt der Erde im Weltbild des frühen Buddhismus

Summary In the gths of the Miglopa-Jtaka and the Gijjha-Jtaka an old Indian narrative is handed down in two basically identical versions which, however, differ from each other, in that the first and older one ascribes a square shape to the earth while the second one conceives it in the form of a wheel. Searching for an explanation for the coexistence of these seemingly contradictory cosmographic pictures in a canonical collection of Buddhist texts, the author of this article discusses in general the archaic cosmological concept of the flat circular disk of the earth, compares relevant sources from vedic and brahmanic literature, and points to some non-Indian tales which are of special interest particularly in regard to the Jtaka versions.     

Geography,migration and abandonment in the Calais refugee camp

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Heterodoxe lehren und ihre widerlegung im Kālacakra-tantra

Summary At the end of the second chapter of the Buddhist Klacakra-Tantra (dated c. 10th century) we find a group of verses in which several doctrines are characterized and criticized: Brahmanism, Vaisnavism, aivism, materialism, Islam and Jainism. Moreover the text refers to Buddhism itself as well as the so-called heterodox Buddhist schools. It is the only old Sanskrit text known until now in which the Islam is mentioned and recognized as a doctrine.     

Human Remains from the Moravian Gravettian: Morphology and Taphonomy of Isolated Elements from the Dolní V stonice II Site

The excavation and palaeoanthropological analysis of the early Upper Palaeolithic site of Dolní V stonice II has yielded a series of incomplete and isolated human remains, comprising cranial vaults, teeth (including a series from an infant), ribs, arm bones, hand phalanges, leg bones, tarsals, metatarsals and pedal phalanges. Morphologically and morphometrically the elements are similar to those from buried individuals at Dolní V stonice I and II and Pavlov I, as well as to other European early Upper Palaeolithic human remains. They differ principally in the high percentage of cortical areas of the distal humerus and femur. The Dolní V stonice 36 infant's teeth may well derive from an undisturbed burial with in situ bone destruction. Geological processes are unlikely to have produced the taphonomic patterns observed, and the preservation and damage patterns of the elements (other than Dolní V stonice 36) suggest that the original bodies were processed by some combination of scavenging agents. Moreover, the original number of burials at Dolní V stonice II may have been greater than the four currently known.