地理科学 ›› 2008, Vol. 28 ›› Issue (2): 247-252.doi: 10.13249/j.cnki.sgs.2008.02.247

• 论文 • 上一篇    下一篇

咸阳市三原县新庄不同植被土层含水量研究

赵景波1,2, 牛俊杰1, 黄芳1   

  1. 1. 陕西师范大学旅游与环境学院, 陕西 西安 710062;
    2. 中国科学院地球环境研究所 黄土与第四纪地质国家重点实验室, 陕西 西安 710075
  • 收稿日期:2007-01-23 修回日期:2007-05-10 出版日期:2008-03-20 发布日期:2008-03-20
  • 作者简介:赵景波(1953-), 男, 山东滕州人, 教授, 博士生导师, 从事环境变迁与自然地理研究。E-mail:zhaojb@snnu.edu.cn
  • 基金资助:
    国家自然科学基金项目(40071006)、中国科学院黄土与第四纪地质国家重点实验室项目(SKLLQG0504)资助。

Changes of Soil Moisture under Different Vegetation in Xinzhuang of Sanyuan,Xianyang City

ZHAO Jing-Bo1,2, NIU Jun-Jie1, DU Juan1   

  1. 1. College of Tourism and Environment Science, Shaanxi Normal University, Xi’an, Shaanxi 710062;
    2. State Key Laboratory of Loess and Quaternary Geology, Environment Institute of Earth, Chinese Academy of Sciences, Xi’an, Shaanxi 710075
  • Received:2007-01-23 Revised:2007-05-10 Online:2008-03-20 Published:2008-03-20

摘要: 通过测定咸阳市三原县新庄2005和2006年降雨正常年份人工林地土壤含水量得知,从地表向下土层含水量呈由高到低再到高的变化;2005年草地和玉米地土层含水量由上向下呈逐渐增高趋势,比同年12龄杨树林地和13龄中国梧桐林地平均含水量高约7%。2003年降水量达880 mm丰水年后,人工林土壤干层中水分完全恢复,人工林出现持续近4年茂盛生长期,预计2007年该区将会再次出现发育弱的土壤干层。

Abstract: According to the measurement of soil moisture underground from zero to six metres of 12-year-old Chinese poplar, 13-year-old Chinese parasol, grassland and the corn land in Xinzhuang Village of Sanyuan, we studied the changes of soil moisture in different soil layers of 0-600 cm under different vegetation. The results show that from the upper to the lower, the soil moisture in artificial forest land changes from high to low, then to high in 2005 and 2006 with normal annual precipitation. The soil moisture in grassland and corn land is about 7% more than that in artificial forest land, and it become more and more downwards. After abundant annual precipitationl of 880 mm in 2003, the average soil moisture in the soil layer of 200-400 cm under 12-year-old Chinese poplar, 13-year-old Chinese parasols in 2005 and 12-year-old Chinese poplar, 13-year-old Chinese parasols in 2006 were higher than those in the dried soil in 2001, which indicates that if the precipitation were increasing, the dried earth layer would become non-dried earth layer. If the annual precipitation were up to 880 mm, the soil moisture could meet the normal growth of artificial forests for about 4 years. Guanzhong Plain and areas with similar annual precipitation are suitable for developing of forests basically. But because of the influence of weak dried earth layer, the forests can’t grow well. According to consuming amount of the soil moisture at 2% per year after the rainy year, weak dried earth layer will appear again under artificial forests in 2007 in Guanzhong Plain if mean annual precipitation is normal. The rainy year is the important supplying period of water for underground water in this area. Water seeping from soil to groundwater is normal in rainy year with a mean annual precipitation about 880 mm and lasting three years after the rainy year.

中图分类号: 

  • S152.7+5