Soil acidity and soil acidification - fundamental concepts and status for five Danish forest soils

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Standard

Soil acidity and soil acidification - fundamental concepts and status for five Danish forest soils. / Raulund-Rasmussen, K.

I: Folia Geographica Danica, Bind 19, 1991, s. 70-82.

Publikation: Bidrag til tidsskrift › Tidsskriftartikel › Forskning › fagfællebedømt

Harvard

Raulund-Rasmussen, K 1991, 'Soil acidity and soil acidification - fundamental concepts and status for five Danish forest soils', Folia Geographica Danica, bind 19, s. 70-82.

APA

Raulund-Rasmussen, K. (1991). Soil acidity and soil acidification - fundamental concepts and status for five Danish forest soils. Folia Geographica Danica, 19, 70-82.

Vancouver

Raulund-Rasmussen K. Soil acidity and soil acidification - fundamental concepts and status for five Danish forest soils. Folia Geographica Danica. 1991;19:70-82.

Author

Raulund-Rasmussen, K. / Soil acidity and soil acidification - fundamental concepts and status for five Danish forest soils. I: Folia Geographica Danica. 1991 ; Bind 19. s. 70-82.

Bibtex

@article{241209db6cb642939789212cc847ce26,
title = "Soil acidity and soil acidification - fundamental concepts and status for five Danish forest soils",
abstract = "Soil acidification is considered the process where protons are neutralized in the soil leading to a decrease in the amount of bases ({"}decrease in acid neutralization capacity'). Soil acidity is both an intensity term (proton activity in the soil solution) and a capacity term (strong base titratable acidity). Acid neutralization by mineral weathering where the products are removed, leads to soil acidification but does not change soil acidity. Soil acidity may be developed, however, when the acid production rate in the soil system exceed the acid neutralization rate. Exchangeable aluminium, sulphate-aluminium, compounds and organic acids are the main sources for soil acidity. Investigations of acid and base properties in five Danish forest soils shows, that in soils with low base contents soil acidification is small but the increase in soil acidity is high, whereas in soils rich in bases soil acidification is high due to leaching of bases but the development of soil acidity is limited. -from Author",
author = "K. Raulund-Rasmussen",
year = "1991",
language = "English",
volume = "19",
pages = "70--82",
journal = "Folia Geographica Danica",
issn = "0071-6693",
publisher = "Kongelige Danske Geografiske Selskab/Royal Danish Geographical Society",

}

RIS

TY - JOUR

T1 - Soil acidity and soil acidification - fundamental concepts and status for five Danish forest soils

AU - Raulund-Rasmussen, K.

PY - 1991

Y1 - 1991

N2 - Soil acidification is considered the process where protons are neutralized in the soil leading to a decrease in the amount of bases ("decrease in acid neutralization capacity'). Soil acidity is both an intensity term (proton activity in the soil solution) and a capacity term (strong base titratable acidity). Acid neutralization by mineral weathering where the products are removed, leads to soil acidification but does not change soil acidity. Soil acidity may be developed, however, when the acid production rate in the soil system exceed the acid neutralization rate. Exchangeable aluminium, sulphate-aluminium, compounds and organic acids are the main sources for soil acidity. Investigations of acid and base properties in five Danish forest soils shows, that in soils with low base contents soil acidification is small but the increase in soil acidity is high, whereas in soils rich in bases soil acidification is high due to leaching of bases but the development of soil acidity is limited. -from Author

AB - Soil acidification is considered the process where protons are neutralized in the soil leading to a decrease in the amount of bases ("decrease in acid neutralization capacity'). Soil acidity is both an intensity term (proton activity in the soil solution) and a capacity term (strong base titratable acidity). Acid neutralization by mineral weathering where the products are removed, leads to soil acidification but does not change soil acidity. Soil acidity may be developed, however, when the acid production rate in the soil system exceed the acid neutralization rate. Exchangeable aluminium, sulphate-aluminium, compounds and organic acids are the main sources for soil acidity. Investigations of acid and base properties in five Danish forest soils shows, that in soils with low base contents soil acidification is small but the increase in soil acidity is high, whereas in soils rich in bases soil acidification is high due to leaching of bases but the development of soil acidity is limited. -from Author

UR - http://www.scopus.com/inward/record.url?scp=0026311838&partnerID=8YFLogxK

M3 - Journal article

AN - SCOPUS:0026311838

VL - 19

SP - 70

EP - 82

JO - Folia Geographica Danica

JF - Folia Geographica Danica

SN - 0071-6693

ER -

ID: 337803230