Results 151 to 160 of about 88,059 (210)

Intercropping tea plants with different leguminous green manures enhances soil nutrient availability, thereby reshaping the structure and functional potential of soil microbial communities. [PDF]

Front Microbiol
Liu Q, Wang LX, Chang PY, Zhang JG, Li C, Shuang QY, Zhang CY, Lu ZK, Wang XL, Jiang XF.   +9 more
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Biological Stability and Microbial Recovery Responses in Vermicomposting of Chemically Intensive Tomato Residues: Defining Management Limits. [PDF]

Toxics
Hepşen Türkay FŞ.
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Experimental soil acidification

Applied Geochemistry, 2002
International ...
Dubikova, M., Cambier, Philippe, P., Caplovicová, M.   +2 more
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Mapping global soil acidification under N deposition

Global Change Biology, 2023
AbstractSoil pH is critically important in regulating soil nutrients and thus influencing the biodiversity and ecosystem functions of terrestrial ecosystems. Despite the ongoing threat of nitrogen (N) pollution especially in the fast‐developing regions, it remains unclear how increasing N deposition affects soil pH across global terrestrial ecosystems.
Chen Chen, Wenya Xiao, Han Y. H. Chen
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Soil Acidification/N Cycling

1991
Publisher Summary In the Dutch Priority Programme on Acidification, soil acidification and related processes have been studied at various sites in forests and heathlands, mostly in association with related research dealing with atmospheric deposition and with various affects of acid deposition on biota.
van Breemen, N., Verstraten, J.M.
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Proton Sinks in Soil Controlling Soil Acidification

1991
This presentation concerns the reaction of the soil and its various constituents with added protons and the ensuing changes induced in the systems’s properties. As these properties largely manifest themselves via the “carrier” agent, the soil solution, it seems logical to use the proton activity in the soil solution, or soil pH value, as the principal ...
Bruggenwert, M.G.M., Hiemstra, T., Bolt, G.H.   +2 more
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Acidification and alkalinization of soils

Plant and Soil, 1983
Acidification or alkalinization of soils occurs through H+ transfer processes involving vegetation, soil solution and soil minerals. A permanent change in the acid neutralizing capacity of the inorganic soil fraction (ANC(s)),i.e. soil acidification (ΔANC 0), results from an irreversible H+ flux. This irreversible H+ flux can be caused either by direct
van Breemen, N., Mulder, J., Driscoll, C.T.   +2 more
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Soil Acidification: Fundamental Concepts

1986
Natural soil acidification processes have been recognized and studied for decades or perhaps centuries. An understanding of these processes is essential to an understanding of soils and of natural and agricultural ecosystems. One of the most important characteristics of soils is the cation-exchange complex.
J. O. Reuss, D. W. Johnson
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