干旱区生态环境知识资源中心(Arid): 干旱半干旱地区砂田结构及水分特征

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	干旱半干旱地区砂田结构及水分特征
其他题名	Soil Profile Structure and Moisture Character of Gravel-Sand Mulched Field in Arid and Semiarid Area of China
	逄蕾; 肖洪浪; 路建龙; 周茂先; 谢忠奎; 李彩芝; 赵良菊; 柴守玺; 常磊; 任娟
来源期刊	中国沙漠
ISSN	1000-694X
出版年	2012
卷号	32 期号:3 页码:698-704
中文摘要	为研究砂田的剖面结构和水分特征,对可用砂田和废弃砂田的剖面结构、土壤含水量、容重和田间最大持水量进行分析测定;建立模拟砂田,研究不同的砾石覆盖条件对土壤水分的影响。结果表明,具有共性的砂田剖面分为5层,分别命名为覆盖层、混合层、根系密集层、淋溶层和钙积层。砾石覆盖可以显著增加土壤含水量,加深淋溶层的下限,剖面结构完整的砂田比结构不完整的砂田的土壤水分状况好。下层土壤含水量显著受上层土壤含水量的影响。以小粒径砾石覆盖且覆盖厚度9cm,最适土壤水分积累。砂田在覆砂的第一年土壤水分含量最低,之后逐渐增加,至覆砂后的6~12a,土壤水分含量达到最高,之后逐渐降低。覆砂后6a左右,土壤容重最小,田间持水量达最大值,此后随着砂田使用年限的增加,土壤容重逐渐增大,田间持水量逐渐减小。
英文摘要	Soil profile,soil moisture content(SMC),soil bulk density and soil water holding capacity both of in-using gravel-sand mulched field(GSMF) and abandoned GSMF in arid and semiarid area were determined to study soil profile structure and soil moisture characters of the GSMF.The effects of different gravel-sand mulching conditions on SMC were also studied through GSMF simulating experiment.The profile of GSMF has five layers,they are gravel-sand mixed layer,soil and gravel-sand mixed layer,roots dense layer,eluviating layer and calcium accumulation layer,respectively.Gravel-sand mulching can increase SMC significantly,and makes the eluviating layer deeper.The soil moisture condition in the GSMF which has full soil profile is better than in the GSMF which hasnt full soil profile.The SMC in upper soil layer is influenced significantly by deeper soil layer.The thickness of 9 cm and the small diameter of gravel-sand can help SMC accumulation.The SMC was the lowest in the first year after gravel-sand mulching,and then it increased slowly with the mulching duration increased.During the mulching year from the sixth to twelfth,the SMC reached the highest level,and then it decreased slowly with the mulching duration increased.When the mulching time is at the sixth year,the soil bulk density reached the lowest,and the water holding capacity reached the highest level,then with the gravel-sand mulching duration increased,the soil bulk density increased and the water holding capacity decreased slowly.
中文关键词	砂田 ; 剖面结构 ; 土壤水分 ; 容重 ; 田间最大持水量
英文关键词	gravel-sand mulched field profile structure soil moisture bulk density water holding capacity
类型	Article
语种	中文
国家	中国
收录类别	CSCD
WOS类目	Agriculture
WOS研究方向	Agriculture
CSCD记录号	CSCD:4542060
来源机构	中国科学院西北生态环境资源研究院 ; 甘肃农业大学
资源类型	期刊论文
条目标识符	http://119.78.100.177/qdio/handle/2XILL650/229018
作者单位	逄蕾, 甘肃农业大学农学院, 甘肃省干旱生境作物学重点实验室, 兰州, 甘肃 730070, 中国.; 肖洪浪, 中国科学院寒区旱区环境与工程研究所, 兰州, 甘肃 730000, 中国.; 周茂先, 中国科学院寒区旱区环境与工程研究所, 兰州, 甘肃 730000, 中国.; 谢忠奎, 中国科学院寒区旱区环境与工程研究所, 兰州, 甘肃 730000, 中国.; 李彩芝, 中国科学院寒区旱区环境与工程研究所, 兰州, 甘肃 730000, 中国.; 赵良菊, 中国科学院寒区旱区环境与工程研究所, 兰州, 甘肃 730000, 中国.; 任娟, 中国科学院寒区旱区环境与工程研究所, 兰州, 甘肃 730000, 中国.; 路建龙, 甘肃农业大学农学院, 兰州, 甘肃 730070, 中国.; 柴守玺, 甘肃农业大学农学院, 兰州, 甘肃 730070, 中国.; 常磊, 甘肃农业大学农学院, 兰州, 甘肃 730070, 中国.
推荐引用方式 GB/T 7714	逄蕾,肖洪浪,路建龙,等. 干旱半干旱地区砂田结构及水分特征[J]. 中国科学院西北生态环境资源研究院, 甘肃农业大学,2012,32(3):698-704.
APA	逄蕾.,肖洪浪.,路建龙.,周茂先.,谢忠奎.,...&任娟.(2012).干旱半干旱地区砂田结构及水分特征.中国沙漠,32(3),698-704.
MLA	逄蕾,et al."干旱半干旱地区砂田结构及水分特征".中国沙漠 32.3(2012):698-704.