Affiliations: Nanjing Institute of Geography & Limnology,
Chinese Academy of Sciences, Nanjing 210008, China | Graduate School of Chinese Academy of Sciences,
Beijing 100039, China
Abstract: Investigation was made into sediment depth at 723 irregularly
scattered measurement points which cover all the regions in Taihu Lake, China.
The combination of successive correction scheme and geostatistical method was
used to get all the values of recent sediment thickness at the 69 × 69
grids in the whole lake. The results showed that there is the significant
difference in sediment depth between the eastern area and the western region,
and most of the sediments are located in the western shore-line and northern
regimes but just a little in the center and eastern parts. The notable
exception is the patch between the center and Xishan Island where the maximum
sediment depth is more than 4.0 m. This sediment distribution pattern is more
than likely related to the current circulation pattern induced by the
prevailing wind-forcing in Taihu Lake. The numerical simulation of
hydrodynamics can strong support the conclusion. Sediment effects on water
quality was also studied and the results showed that the concentrations of TP,
TN and SS in the western part are obviously larger than those in the eastern
regime, which suggested that more nutrients can be released from thicker
sediment areas.
Keywords: objective analysis, geostatistics, sediment distribution, Taihu Lake