SOME BANDED SOILS OF SOUTHERN VELUWE (NETHERLANDS)

被引：2

作者：

SEVINK, J

VINK, APA

机构：

[1] Fysisch Geografisch en Bodemkundig Laboratorium, University of Amsterdam, Amsterdam

来源：

GEODERMA | 1969年 / 3卷 / 02期

关键词：

D O I：

10.1016/0016-7061(69)90011-1

中图分类号：

S15 [土壤学];

学科分类号：

0903 ; 090301 ;

摘要：

The loess cover in the region of Middachten near Arnhem is of the Last Glacial Age. An investigation of four profile-pits showed that, during the deposition of the loess, tundra soils with a thin Bt-horizon were formed. Solifluction and fresh deposits on these soils resulted in the formation of a series of loess layers, each showing more or less strongly developed flowstructures as well as remnants of Bt-horizons disturbed by the subsequent flowage-phenomena. Several of these profiles show fragipan-characteristics. The authors suggest a close relation between the formation of the fragipans and the occurrence of periglacial tundra climates. © 1969.

引用

页码：157 / &

共 20 条

[1]

BOUMA J., 1968, NETH J AGR SCI, V16, P58

[2]

CARLISLE F. J., 1957, Soil Science Society of America. Proceedings, V21, P320

[3]

CROMMELIN RD, 1965, BOOR SPADE, V14, P138

[4]

De Bakker H., 1966, SYSTEEM BODEMCLASSIF

[5]

DUDAL R, 1968, DEFINITIONS SOIL UNI

[6]

GROSSMAN R. B., 1957, Soil Science Society of America. Proceedings, V21, P322

[7]

HEBERT J, 1964, 8 T INT C SOIL SCI, V5, P359

[8]

JHA P. P., 1963, SOIL SCI SOC AMER PROC, V27, P339

[9]

KARAVAEVA NA, 1964, 8 T INT C SOIL SCI, V5, P501

[10]

KNOX ELLIS G., 1957, SOIL SCI SOC AMER PROC, V21, P326

← 1 2 →