[1]赵景波,张慧慧,马淑苗,等.青海湖沙柳河镇南部土壤入渗规律[J].山地学报,2013,(06):693.
　ZHAO Jingbo,ZHAO Huihui,MA Shumiao.Soil Infiltration Rule in Southern Shaliuhe Town of Qinghai Lake Area[J].Mountain Research,2013,(06):693.
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青海湖沙柳河镇南部土壤入渗规律()
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《山地学报》[ISSN:1008-2186/CN:51-1516]

卷:
期数:
2013年06期
页码:
693
栏目:
山地环境
出版日期:
2013-01-01

文章信息/Info

Title:
Soil Infiltration Rule in Southern Shaliuhe Town of Qinghai Lake Area
作者:
赵景波;张慧慧;马淑苗;
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
Author(s):
ZHAO Jingbo; ZHAO Huihui; MA Shumiao
1.Tourism and Environment College, Shaanxi Normal University, Xi’an 710062, China;
2.State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, CAS, Xi’an 710075, China
关键词:
土壤入渗率; 低草地; 高草地; 油菜地; 青海湖北部
Keywords:
soil infiltration;  low grassland;  high grassland;  rape field;  north Qinghai Lake
分类号:
P641,S152
文献标志码:
A
摘要:
通过对青海湖北部沙柳河镇不同植被类型土壤入渗实验测定,研究了不同植被类型土壤入渗特征及土壤蓄水性。结果表明,青海湖农场四大队厚土层低草地、高草地、油菜地和沙柳河镇南薄土层低草地的初渗率均值分别为4.55、4.71、0.64和2.31 mm/min,稳定前平均入渗率均值分别为2.09 mm/min、3.29 mm/min、0.53 mm/min和1.95 mm/min,稳渗率均值分别为1.53 mm/min、2.31 mm/min、0.32 mm/min和1.74 mm/min。在同一实验区,不同植被类型的土壤入渗率为高草地>低草地>油菜地。同种植被厚土层的初渗率大于薄土层,而厚土层的稳定前平均...
Abstract:
Through the determination of soil infiltration experiments on different vegetation types in southern Shaliuhe Town of Qinghai Lake area, the characteristics of the soil infiltration and the water maintenance in soil of different vegetation types were analyzed. The result showed that the mean values of initial infiltration rate of low grasslands, high grasslands and rape fields of thick soil in the fourth group of Qinghai Lake Farm and low grasslands of thin soil in southern Shaliuhe town were separate 455, 471, 064 and 231 mm/min. Average infiltration before stability were 209, 329, 053 and 195 mm/min respectively. The steady soil infiltration was 153, 231, 032 and 174 mm/min separately. In the same land, soil infiltration of high grasslands was highest. The soil infiltration of rape fields was lowest. The soil infiltration of low grasslands was intermediate. The time at which soil infiltration comes to a steady state was different among different vegetation types and soil thickness. Horton formula was a better one for fitting the experimental data, and the applicability of Koctakob formula and general empirical formula was bad in the study area. Soil porosity and the porosity among soil particle of southern Qinghai Lake were bigger than Shaanxi Loess Plateau’s, which led to that steady soil infiltration of southern Qinghai Lake was higher that of Shaanxi Loess Plateau. The characteristics of small soil thickness, low capacity of soil reservoir and little storage capacity in the study area determined the fragile ecological environment and grassland degradation easily occurred in drought years.

备注/Memo

备注/Memo:
收稿日期(Received date)：2013-02-07；改回日期(Accepted) : 2013-05-20。
基金项目（Foundation item）：国家科技支撑计划项目（2007BAC30B01）；中国科学院黄土与第四纪地质国家重点实验室项目（SKLLQG1214）。[The Ministry of national science and technology support program（2007BAC30B01）; Project of State Key Laboratory of Loess and Quaternary Geology, CAS, No. SKLLQG1214.]
作者简介（Biography）：赵景波(1953-)，男，山东滕州人，博士，教授，博士生导师，主要从事第四纪与环境科学研究。[Zhao Jingbo(1953-)，Ph. D. and Professor, specialized in Quaternary and environmental science.] E-mail: zhaojb@snnu.edu.cn
更新日期/Last Update: 1900-01-01