Field investigations of soil hydrological properties of fen soils in North-East Germany

被引：8
|
作者：
Schindler, U
Müller, L
Behrendt, A
机构：
[1] ZALF Muncheberg, Inst Bodenlandschaftsforsch, D-15374 Muncheberg, Germany
[2] ZALF Munchenberg, Forsch Stn Landwirschaft Paulinenaue, D-14641 Paulinenaue, Germany
来源：
JOURNAL OF PLANT NUTRITION AND SOIL SCIENCE | 2003年 / 166卷 / 03期
关键词：
fen soil; soil development; soil hydrological properties; capillary rise; pore space distribution;
D O I：
10.1002/jpln.200390056
中图分类号：
S3 [农学（农艺学）];
学科分类号：
0901 ;
摘要：
To investigate the changes of hydrological properties of peat soil in course of soil development, field measurements at 84 fen sites (Histosols) in 19 fen regions of North-East Germany were carried out. Capillary water supply at all the stages of soil development was not limited up to 70 cm of ground water level. Worsening of plant water supply was the result of mud accumulation in the capillary fringe, ground water levels located deeper than 70 cm below soil surface, low hydraulic conductivity in the ground water zone, and hysteresis effects, affected by high dynamics of ground water level during the day.
引用
收藏
页码：364 / 369
页数：6
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