Multiparametric analysis of soil properties in the drained forest bogs of Western Siberia

被引：0
|
作者：
T. T. Efremova
T. M. Ovchinnikova
V. G. Sukhovol’skii
机构：
[1] Russian Academy of Sciences,Sukachev Institute of Forestry, Siberian Division
来源：
Eurasian Soil Science | 2006年 / 39卷
关键词：
EURASIAN Soil Science; Water Regime; Groundwater Table; Hydrological Regime; Canonical Correlation;
D O I：
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中图分类号：
学科分类号：
摘要：
The application of multiparametric statistical methods has confirmed that peat soils are different in the degree of their drainage and properties because of their modification during a 20–25 year period of artificial drainage operation. The following sequence represents the relative significance of the contribution to the soil changes of the parameters studied: groundwater table > air capacity > pH > 0T > Eh > water-soluble: C > Fe3+ > NH4+ and the activity of soil oxidoreductases in the following sequence: peroxidase > catalase > dehydrogenase. The necessity to supplement the substantive-genetic principle of the classification of drained peat soils with characterization of their water regime is substantiated.
引用
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页码：588 / 596
页数：8
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