1. 中国科学院 南京地理与湖泊研究所 湖泊与环境国家重点实验室,江苏,南京,210008
2. 南京市地产发展中心,江苏,南京,210005
纸质出版:2014
移动端阅览
徐飞, 朱青, 史伯强, 等. 太湖流域平原区土壤水分动态分析[J]. 水土保持通报, 2014,33(6):54-58.
XU Fei, ZHU Qing, SHI Bo-qiang, et al. Dynamic Analysis of Soil Water in Plain Area of Taihu Lake Basin[J]. Bulletin of Soiland Water Conservation, 2014, 33(6): 54-58.
徐飞, 朱青, 史伯强, 等. 太湖流域平原区土壤水分动态分析[J]. 水土保持通报, 2014,33(6):54-58. DOI: 10.13961/j.cnki.stbctb.2014.06.017.
XU Fei, ZHU Qing, SHI Bo-qiang, et al. Dynamic Analysis of Soil Water in Plain Area of Taihu Lake Basin[J]. Bulletin of Soiland Water Conservation, 2014, 33(6): 54-58. DOI: 10.13961/j.cnki.stbctb.2014.06.017.
以太湖流域平原区两种土地利用方式(林地和菜地)为例
在长期定位观测土壤水分数据的基础上
采用时间序列法定量分析了土壤水分与降水之间的相关关系。结果表明:(1)降水量在时间上不相关
而各层土壤水分均为自相关序列;(2)降水与土壤水分之间存在一定的相关性
相关时长受季节、土壤深度、土地利用方式等的影响较为明显(1~8 d不等);(3)林地相关时长的季节变化表现为:夏秋季 >春季 >冬季。随着土壤深度的增加
菜地土壤含水量与降水相关关系在夏秋季节呈减小趋势
而在冬春季节则相反。整体上林地降水对土壤含水量的有效影响时间长于菜地
且林地降水量与土壤含水量相关关系的规律性优于菜地。
Based on the long time monitoring data
taking the two typical land-use types(vegetable land and forest) in the plain of Taihu Lake basin as an example
the correlation between soil moisture and precipitation was analyzed with the time series method. The results showed that:(1) Precipitation time series was temporally uncorrelated
soil moisture contents in different depths
however
were self-correlation series.(2) There was a relationship existed between soil moisture and precipitation
the related time was in the range of 1~8 days due to the influence of seasons
soil depths and land-use types.(3) The seasonal change of the related time in forest can be described as:summer and autumn >spring >winter. With the increase of soil depth
the relationship between soil moisture and precipitation showed a trend of decrease in summer and autumn. The correlation in winter and spring
however
were the opposite. In conclusion
the effective time of precipitation on soil moisture was longer in forest than in vegetable land
and the regularity of the relationship between soil moisture and precipitation in forest was much better than that in the vegetable land.
张超,王会肖.土壤水分研究进展及简要评述[J].干旱地区农业研究,2003,21(4):117-125.
Seneviratne S I, Corti T, Davin E L, et al. Investigating soil moisture-climate interactions in a changing climate[J].Earth-Science Reviews, 2010,99(3):125-161.
邵晓梅,严昌荣,徐振剑.土壤水分监测与模拟研究进展[J].地理科学进展,2004,23(3):58-66.
秦伯强.太湖生态与环境若干问题的研究进展及其展望[J].湖泊科学,2009,21(4):445-455.
李恒鹏,刘晓玫,黄文钰.太湖流域浙西区不同土地类型的面源污染产出[J].地理学报,2004,59(3):401-408.
石辉,刘世荣,孙鹏森,等.黄土丘陵区人工油松林地土壤水分动态的时间序列分析[J].山地学报,2004,22(4):411-414.
宋献方,王仕琴,肖国强,等.华北平原地下水浅埋区土壤水分动态的时间序列分析[J].自然资源学报,2011,26(1):145-155.
王晓燕,陈洪松,王克林,等.红壤坡地土壤水分时间序列分析[J].应用生态学报,2007,18(2),297-302.
王贺年,余新晓.北京山区林地土壤水分时间序列分析[J].山地学报,2012,30(5):550-554.
傅伟,王克林,陈洪松,等.典型峰丛洼地坡面土壤水分动态变化的时序分析[J].水土保持学报,2005,19(4):111-114.
高俊峰,闻余华.太湖流域土地利用变化对流域产水量的影响[J].地理学报,2002,57(2):194-200.
周刘宗,陈志雄,雷志栋,等.土壤水分的时序分析研究[J].土壤,1998(4):188-193.
蒋太明,刘海隆,刘洪斌.黄土坡地土壤水分入渗垂直变异特征分析[J].水土保持学报,2004,18(3):49-52.
张丽丽,陈家宙,吕国安,等.利用土壤表层含水量序列预测深层含水量的研究[J].水土保持学报,2007,21(3):162-169.
0
浏览量
1447
下载量
0
CSCD
关联资源
相关文章
相关作者
相关机构
京公网安备11010802024621