Taking Xinjiang Weigan River irrigation district as an example, 38 observation wells’ data from 1997 to 2007 of groundwater depth and groundwater mineralization were used in the paper to analyze annual change of groundwater depth and the groundwater mineralization of Weigan River irrigation district, and their seasonal dynamics and spatial distribution. The results showed that in the 11 years period, the highest groundwater level appeared in spring. The groundwater level rose significantly from the top of irrigation district to the periphery of the oasis. The overall trend of groundwater mineralization is that groundwater mineralization is relatively low in the upper reaches of the irrigation district, and relatively high in the lower edge and downstream of the irrigation district. The annual groundwater depth and groundwater mineralization generally decreased in the irrigation district.
TURSUN·Hasan, TASHPOLAT·Tiyip, MAMAT·Gazat, MAMTIMIN·Mamat
. Spatial and Temporal Dynamic Distribution of Groundwater Depth and Mineralization in Weigan River Irrigation District[J]. SCIENTIA GEOGRAPHICA SINICA, 2011
, 31(9)
: 1131
-1137
.
DOI: 10.13249/j.cnki.sgs.2011.09.1131
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