Open Access
Methods of soil analysis.
Arnold Klute,Dwayne R. Buxton editor-in-chief Asa publications,John J. Mortvedt. editor-in-chief Sssa publications +2 more
- 22 Apr 2015
Iss: 1
8.5K
About: The article was published on 22 Apr 2015. and is currently open access. The article focuses on the topics: Soil morphology & Soil series.
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Citations
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References
Analysis of factors controlling soil organic matter levels in Great Plains grasslands
TL;DR: In this article, a model of soil organic matter (SOM) quantity and composition was used to simulate steady-state organic matter levels for 24 grassland locations in the U.S. Great Plains.
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TL;DR: In this paper, the authors present a modeling approach aimed at seasonal resolution of global climatic and edaphic controls on patterns of terrestrial ecosystem production and soil microbial respiration using satellite imagery (Advanced Very High Resolution Radiometer and International Satellite Cloud Climatology Project solar radiation), along with historical climate (monthly temperature and precipitation) and soil attributes (texture, C and N contents) from global (1°) data sets as model inputs.
Climatic, edaphic, and biotic controls over storage and turnover of carbon in soils
David S. Schimel,Bobby H. Braswell,Elisabeth A. Holland,Rebecca McKeown,Dennis S. Ojima,Thomas H. Painter,William J. Parton,Alan R. Townsend +7 more
TL;DR: In this paper, the Century ecosystem model was applied to a series of forest and grassland sites distributed globally to examine large-scale controls over soil carbon, including soil texture and foliar lignin content.
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TL;DR: In this article, the Rothamsted model is used to calculate the amount of CO2 that would be released from the world stock of soil organic matter if temperatures increase as predicted, the annual return of plant debris to the soil being held constant.
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The role of biology in the formation, stabilization and degradation of soil structure
TL;DR: In this paper, the formation of soil structure involves the physical forces of shrinking and swelling created by changes in water status of soils, freezing and thawing, tillage, or by movement of the larger biota in soils.
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