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Soil and the Anthropocene | 34147
Journal of Geology & Geophysics

Journal of Geology & Geophysics
Open Access

ISSN: 2381-8719

+44 1478 350008

Soil and the Anthropocene


International Conference on Geosciences and Geophysics

October 06-07, 2016 Orlando, USA

Rattan Lal

The International Union of Soil Science, Austria
Ohio State University, USA

Posters & Accepted Abstracts: J Geol Geophys

Abstract :

The so-called â�?�?Anthropoceneâ�? may have been set-in-motion with the dawn of settled agriculture about 10 millennia ago, but accelerated with the onset of Industrial Revolution ~circa 1750. An increase in access to food through settled agriculture increased human population (billion) from 0.002-0.02 during the hunter/gatherer era to ~1 in 1800, 1.7 in 1900, 2.5 in 1950, 6.1 in 2000, 7.5 in 2016 and projected to 9.7 by 2050 and 11.2 by 2100. The environmental impact (I=PAT, where P is population, A is affluence and T is technology) includes deforestation, alterations of biogeochemical cycling of elements (C, N, P) and water, soil degradation (erosion, salinization, C and nutrient depletion), loss of biodiversity, eutrophication of natural water and global climate change. Atmospheric concentration of CO2 increased from ~280 ppm around 1750 to>400 ppm at present, along with increase in concentration of other radiatively-active gases including CH4 (722 ppb to 1883 ppb) and N2O (270 ppb to 327 ppb). The magnitude of C emitted into the environment from pre-historic era to 2010 is estimated at 456 Pg compared with that of 200 Pg from fossil fuel combustion. Presently, 38% of Earthâ�?�?s land surface is used for agriculture, 70% of the global fresh water withdrawal is used for irrigation, and 30-35% of global greenhouse gas emissions are contributed by agriculture. Yet, 1 in 7 persons are food-insecure and 2-3 in 7 are malnourished. Nonetheless, soil matters, because solution to global issues lies in sustainable intensification of soil by producing more from less.

Biography :

Email: lal.1@osu.edu

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