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Grown primarily by the smallholder farmers in tropical and subtropical regions, pigeonpea is pivotal to subsistence agriculture in Aisa, Africa, Latin America and the Caribbean. Last two decades have witnessed several research breakthroughs in pigeonpea.
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This guide examines geophysical methods for geothermal energy exploration, covering techniques like seismic... Læs mere
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Subsurface Remediation: Vadose Zones and Aquifers presents state-of-the-art physical treatment methods for remediating contaminated subsurface formations, bridging theoretical foundations with practical applications through pedagogically enriched content.
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Environmental planning is the integrated analysis and assessment of the surroundings environmental information into the planning process for development. This book provides a detailed account of the multi-faceted and interdisciplinary aspects of environmental planning.
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Oceanic basalts are the most abundant rock type found at the Earth's surface. This book provides a review of these rocks, first discussing how we sample the ocean floor and what we know... Læs mere
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X-ray crystallography provides us with the most accurate picture we can get of atomic and molecular structures in crystals. It is still an immense field for young workers, and no doubt will provide yet more striking developments of a major character.
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The inner core consists mostly of iron and its temperature is about 5000 kelvin, whereas the liquid outer core is turbulent, rotates faster than the mantle, consists primarily of iron, and is the source of the Earth's magnetic field.
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A collection of 17 papers by authors from diverse backgrounds dealing with multi-disciplinary research on the Patagonian ice fields. The main emphasis is glaciology, climatology and paleoclimatology, with contributions in glacier ecology, microbiology and aerosols.
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Most of our knowledge about the physical structure and the chemical composition of the Earth's deep interior is inferred from seismic data.
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Introduces Fredholm integral equations that are suited to the numerical solution of boundary value problems representing the electrical, magnetic, electromagnetic and seismic models of geophysics. The approach adopted is physical rather than mathematical.