黄河三角洲农田灌溉前后土壤盐分时空变异特征研究

CORC > 烟台海岸带研究所 > 中国科学院烟台海岸带研究所 > 中科院海岸带环境过程与生态修复重点实验室

	黄河三角洲农田灌溉前后土壤盐分时空变异特征研究
	吴向东 ; 陈小兵 ; 吕真真 ; 郭建青 ; 于君宝
刊名	干旱地区农业研究
	2013-05
卷号	31 期号:3 页码:194-199+243
关键词	土壤含盐量灌溉时空变异特征半方差函数田块尺度盐碱地
其他题名	Spatia-l temporal variability of soil salt content before and after irrigation in the Yellow River Delta
通讯作者	陈小兵 E-mail:xbchen@yic.ac.cn
产权排序	安徽淮河水资源科技有限公司;中国科学院烟台海岸带研究所;中国科学院南京土壤研究所;长安大学
中文摘要	分别采用传统统计学和地统计学方法,定量分析了灌溉前、后黄河三角洲田块尺度下不同深度土层含盐量的空间变异性并分析空间分布特征。结果表明:除灌溉前0~10 cm土层土壤含盐量呈强变异性外,其余各土层含盐量均表现为中等变异强度;灌溉前土壤盐分主要积聚在0~10 cm和40~60 cm土层,灌溉后主要积聚在40~60 cm土层;灌溉使得0~10 cm和10~20 cm土层土壤含盐量降低,脱盐效果较好;除灌溉后0~10 cm土层的土壤盐分含量呈现弱空间相关性之外,其它土层均呈现强空间相关性;灌溉后与灌溉前相比,除40~60 cm层土壤含盐量外,其余各土层土壤含盐量明显降低、土壤含盐量的等值线密集程度减弱...
英文摘要	In attempt to study spatial and temporal variability of soil salt content before and after irrigation, the descriptive statistics and geostatistics were used to quantitatively analyze soil salt content of field-scale in vertical and hor-i zontal directions in the Yellow River Delta. The result showed that soil salt content was gathered in 0~ 10 cm layer and 40~ 60 cm layer before the irrigation, and gathered in 40~ 60 cm layer after the irrigation. Irrigation reduced salinity of 0~ 10 cm and 10~ 20 cm soil layer and gained better desalination. Except soil salt content of 0~ 10 cm layer had a weak spatial correlation after irrigation, all other layers of soil showed a strong spatial correlation. Compared salt content of soil before irrigationwith after irrigation, salt content of 40~ 60 cm layer was significantly reduced after irrigation, soil salinity contour intensity was weakened, and spatial distribution trend clearly turned to flat. Before irrigation, high soil salinities of all soil layerswere detected in the northern part of the study area, while low soil salinities were detected in the northwest corner; After irrigation, except high soil salinity of 0~ 10 cm layer was detected in north-central area, high soil salinities of the rest layers( 10~ 20 cm, 20~ 40 cm and 40~ 60 cm) were discovered in south-central or central area. Low soil salinity of each layer of soil showed same distribution pattern, and they were mostly observed in the northern part of the experimental field.
学科主题	农学
收录类别	CSCD
资助信息	公益性行业(农业)科研专项经费项目(200903001);; 黄河三角洲生态环境重点实验室(2008KFJJ03);; 海洋公益性行业科研专项(201105020);; 国家科技支撑计划项目(2009BADA3B04)
CSCD记录号	CSCD:4867665
公开日期	2013-08-13
内容类型	期刊论文
源URL	[http://ir.yic.ac.cn/handle/133337/6375]
专题	烟台海岸带研究所_中科院海岸带环境过程与生态修复重点实验室
推荐引用方式 GB/T 7714	吴向东,陈小兵,吕真真,等. 黄河三角洲农田灌溉前后土壤盐分时空变异特征研究[J]. 干旱地区农业研究,2013,31(3):194-199+243.
APA	吴向东,陈小兵,吕真真,郭建青,&于君宝.(2013).黄河三角洲农田灌溉前后土壤盐分时空变异特征研究.干旱地区农业研究,31(3),194-199+243.
MLA	吴向东,et al."黄河三角洲农田灌溉前后土壤盐分时空变异特征研究".干旱地区农业研究 31.3(2013):194-199+243.