[Soil condensation water in different habitats in Horqin sandy land: an experimental study].
Weighing method was adopted to study the formation time and the amount of soil condensation water in four habitats (mobile sandy land, fixed sandy land, farmland, and Mongolian pine forest land) in Horqin Sandy Land in August 2007. The soil condensation water began to form at 20:00-22:00, increased gradually at 22:00-4:00, and began to evaporate after 4:00. In the four habitats, soil condensation water was mainly formed in 0-9 cm layer, and the amount was the greatest in 0-3 cm layer, accounting for 40% of the total. The soil condensation water also formed in 9-30 cm layer, but in very small amount. There was a greater difference in the mean daily amount of soil condensation water in 0-3 cm layer in the four habitats, with the sequence of fixed sandy land > mobile sandy land > farmland > Mongolian pine forest land, which indicated that the habitat with better vegetation condition was not benefit the formation of soil condensation water. The mean daily amount of soil condensation water in 0-30 cm layer was 0.172 mm in fixed sandy land, 0.128 mm in Mongolian pine forest land, 0.120 mm in mobile sandy land, and 0.110 mm in farmland.
Liu
Xin-Ping
XP
Naiman Desertification Research Station, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou, China. xpliuhyh@126.com
He
Yu-Hui
YH
Zhao
Xue-Yong
XY
Li
Yu-Lin
YL
Li
Yu-Qiang
YQ
Li
Yan-Qing
YQ
Li
Shi-min
SM
D002681:China; D018556:Crops, Agricultural / Q000254:growth & development*; D003889:Desert Climate; D017753:Ecosystem; D028223:Pinus / Q000254:growth & development*; D012822:Silicon Dioxide; D012987:Soil / Q000032:analysis*; D014867:Water / Q000032:analysis*
D012987:Soil; D014867:Water; D012822:Silicon Dioxide