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黄土高原生物结皮对土壤水分入渗的影响

张侃侃 卜崇峰 高国雄

干旱区研究2011,Vol.28Issue(5):808-812,5.
干旱区研究2011,Vol.28Issue(5):808-812,5.

黄土高原生物结皮对土壤水分入渗的影响

Effect of Microbiotic Crust on Soil Water Infiltration in the Loess Plateau

张侃侃 1卜崇峰 1高国雄2

作者信息

  • 1. 西北农林科技大学资源与环境学院,陕西杨凌712100
  • 2. 中国科学院水利部水土保持研究所,陕西杨凌712100
  • 折叠

摘要

Abstract

In this study,the disc infiltrometers were used to measure soil water infiltration under 6 kinds of treatments(the regions where there was no microbiotic crust,there was microbiotic crust,Stipa bungeana grows,S.bungeana grows with microbiotic crust,Korshinsk peashrub grows,K.peashrub grows with microbiotic crust),and the measured data were compared and analyzed.The results are as follows:(1) Microbiotic crust impeded soil water infiltration whether there was vegetation or not,and the stable infiltration rate and cumulative infiltration were higher in the regions where there was no microbiotic crust than those in the regions where there was microbiotic crust;vegetation increased the capability of resisting soil water infiltration of microbiotic crust;(2) The fitting effect with Kostiakov model under the treatment without microbiotic crust and with S.bungeana was fine;that with Philip model under the treatments without microbiotic crust,with K.peashrub and K.peashrub with S.bungeana was fine;and that of water infiltration with Horton model under all 6 kinds of treatments was fine.Therefore,Horton model can be used to describe soil water infiltration in the Loess Plateau.

关键词

生物结皮/土壤水分/入渗速率/累积入渗量/入渗模型/神木县/陕西/黄土高原

Key words

microbiotic crust/soil moisture cointent/infiltration rate/cumulative infiltration/infiltration model/Shenmu County/Shaanxi Province/Loess Plateau

分类

农业科技

引用本文复制引用

张侃侃,卜崇峰,高国雄..黄土高原生物结皮对土壤水分入渗的影响[J].干旱区研究,2011,28(5):808-812,5.

基金项目

国家自然科学基金项目(40701096) (40701096)

中国科学院西部之光(B28013200) (B28013200)

西北农林科技大学科研专项(QN2009085) (QN2009085)

干旱区研究

OA北大核心CSCDCSTPCD

1001-4675

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