欢迎访问《中国农学通报》,

中国农学通报 ›› 2010, Vol. 26 ›› Issue (3): 188-195.

• 资源 环境 生态 土壤 气象 • 上一篇    下一篇

安塞黄土丘陵区人工草地生产力与土壤水分特征

姜峻1,王百群1,曹清玉1,都全胜2   

  • 收稿日期:2009-09-07 修回日期:2009-09-22 出版日期:2010-02-05 发布日期:2010-02-05

Characteristics and the Biomass Production and Soil Water of Sown Pastures in Ansai Loess hilly-gully Region

  • Received:2009-09-07 Revised:2009-09-22 Online:2010-02-05 Published:2010-02-05

摘要:

摘 要 人工草地建设是半干旱黄土丘陵区生态建设与农业生产的重要组成部分,比较不同类型人工草地生产力、土壤水分差异,可为草地建设中草地类型的选择与管理提供依据。通过比较川地与山地不同类型草地生产力、土壤水分年季变化差异,表现为以下特征:川地人工草地0-100cm土壤含水量受季节降雨量影响变化较为活跃,为活跃层。100-350cm土壤含水量与根系利用有关,为次活跃层。350-500cm季节变化不大,为相对稳定层。柳枝稷与苜蓿草地350-500cm土层干燥化明显。在2004-2005年,各草地4月到9月0-200cm土壤储水量减少,9月到11月0-200cm储水量增加,200cm以下各草地间差异明显,但季节变化量接近。山坡不同类型草地0-100cm土壤含水量表现为秋末高于春季,100-500cm不同季节均未显示明显的水分亏缺现象。

关键词: CO2浓度, CO2浓度, 碳水化合物, 产量, 水稻

Abstract:

ABSTRACT Sown pasture is an important part of ecological construction and agricultural production in semiarid loess hilly-gully region. It is also important for selecting proper sown pasture types and management methods after comparing the biomass production, soil water contents of different sown pastures. The yearly change of the biomass production, soil water and nutrient content were compared between lowland and slopland at Ansai loess hilly-gully region. Soil water characteristics of sown pastures: The change of soil water content in 0-100cm soil depth of lowland sown pasture was more active, and which was the active layer; soil water content in 100-350cm soil depth was related with the root system consumption, and was hypo-active layer; the seasonal change of soil water content in 350-500cm was small, and which was relatively stable layer. The soil drying phenomenon was distinctive in 350-500cm soil layer of switchgrass and alfalfa. In 2004-2005, the soil water storage in 0-200cm decreased from Aril to September, while increased from September to November. There were great differences among pastures in soil depth below 200cm, but the seasonal change was similar. The 0-100cm soil water content in late autumn was higher than in springtime at slope pasturelands, and there were no evident soil water stress in 100-500cm in each pastureland.