神府东胜煤田复垦区土壤入渗特性的试验研究


Autoria(s): 付微; 邵明安; 黄明斌
Data(s)

2008

Resumo

土壤入渗性能是最基本的土壤物理特性之一。复垦区土壤的结构组成复杂,入渗特性有别于非矿区土壤。本文以神府东胜煤田马家塔复垦区为研究对象,利用圆盘入渗仪分别测定了复垦区乔木、林地、荒地、灌木林地和草地的土壤入渗特性,用经典统计学方法对复垦区土壤入渗性能的空间变异性进行了分析。实测结果表明,不同土地利用方式下的土壤入渗特性有较大的差异;在测定范围内,乔木林地、荒地、草地和灌木林地的稳定入渗率均表现出0 cm>—3 cm>—15 cm的规律性,其中草地稳定入渗率随吸力的变化更明显。研究表明:乔木林地稳定入渗率和累积入渗量的变异系数分别为0.58和0.49.属于中等变异。

Soil infiltrability is one of most important soil physical properties.The structure and texture of the soils in reclamation areas are quite complex,which results in different infiltration properties from the non- reclamation ones.In this study,disc permeameter was employed to measure soil infiltration properties for different land use types in the Majiata reclamation area of Shenmu-Fugu Dongsheng coal mine.The land use types are:woodland,wild-land,shrub-land,and grassland.The results showed that significant...

Identificador

http://ir.iswc.ac.cn/handle/361005/580

http://www.irgrid.ac.cn/handle/1471x/140179

Idioma(s)

中文

Fonte

付微, 邵明安, 黄明斌.神府东胜煤田复垦区土壤入渗特性的试验研究.水土保持学报,2008,3:14-17

Tipo

期刊论文