干旱区生态环境知识资源中心(Arid): 干旱区农田土壤水分地温变化规律及其相互关系

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	干旱区农田土壤水分地温变化规律及其相互关系
其他题名	The variation rule and interrelationship of farmland soil moisture content and ground temperature in arid areas
	张建兵 1; 熊黑钢2 ; 李宝富 3; 龙桃 4
来源期刊	干旱地区农业研究
ISSN	1000-7601
出版年	2013
卷号	31 期号:2 页码:127-133
中文摘要	以干旱区农田灌溉后土壤水分、地温实测数据为基础,研究了其土壤水分、地温各自的变化规律及两者的相互关系。结果表明,各层含水量之间具有高相关性,基本达到了极显著的水平。这与土壤水分灌溉时由上而下的逐渐下渗,以及蒸发时由下而上的逐层上升有密切的关系。各层地温间的相关性大,除地面温度外,其余各层地温间的相关水平为显著或极显著水平,且相邻土层地温间均呈极显著相关。土壤水分及地温剖面垂直变化特征明显,并具有动态性。土壤水分含量大时,两者的垂直变异系数小,反之变异系数大。0~20 cm、地面(0 cm)分别为剖面含水量及地温变异强度的最大层,属中等变异强度。土壤水分及温度之间的负相关性明显。地面温度是预测表层、底层土壤水分的良好指标,利用回归分析法建立的土壤水分与地温间的函数关系可为推测土壤水分提供依据。
英文摘要	Based on the data of irrigated farmland soil moisture content and ground temperature, this paper studied their variation rules and coupling relationships. The results showed that soil moisture content of each layer correlated significantly because the soil water infiltrated from top to bottom layer by layer when irrigation, and reversed when evaporation. The correlation of each layer ground temperature was obvious. Except for land surface temperature, ground temperature of soil layers had significant correlations especially the adjacent soil layers. The vertical variation characters of soil moisture content and ground temperature were distinct and dynamic. When it comes to high soil moisture content, their vertical variation coefficient was small; however variability became bigger when soil moisture content decreased. Both of the land surface ground temperature and soil moisture of 0 ~ 20 cm soil layer had middle variation, which is the highest variation of ground temperature and soil moisture content. Soil moisture content and ground temperature had obviously negative correlation. Land surface temperature was a good factor to forecast soil moisture content of the top and bottom soil layer. The linear regression equation of soil moisture content and ground temperature could be helpful for soil moisture content forecasting.
中文关键词	土壤水分 ; 地温 ; 相互关系 ; 干旱区
英文关键词	soil moisture content soil temperature interrelationship arid area
语种	中文
国家	中国
收录类别	CSCD
WOS类目	AGRICULTURE MULTIDISCIPLINARY
WOS研究方向	Agriculture
CSCD记录号	CSCD:4813845
来源机构	中国科学院新疆生态与地理研究所
资源类型	期刊论文
条目标识符	http://119.78.100.177/qdio/handle/2XILL650/229473
作者单位	1.中国科学院南京土壤研究所, 南京, 江苏 210008, 中国; 2.北京联合大学应用文理学院, 教育部绿洲重点实验室, 北京 100083, 中国; 3.中国科学院新疆生态与地理研究所, 乌鲁木齐, 新疆 830011, 中国; 4.重庆市永川区国土资源和房屋管理局, 重庆 402160, 中国
推荐引用方式 GB/T 7714	张建兵,熊黑钢,李宝富,等. 干旱区农田土壤水分地温变化规律及其相互关系[J]. 中国科学院新疆生态与地理研究所,2013,31(2):127-133.
APA	张建兵,熊黑钢,李宝富,&龙桃.(2013).干旱区农田土壤水分地温变化规律及其相互关系.干旱地区农业研究,31(2),127-133.
MLA	张建兵,et al."干旱区农田土壤水分地温变化规律及其相互关系".干旱地区农业研究 31.2(2013):127-133.