Abstract

A geophysical survey was carried out for Taihu Lake, one of the largest shallow lakes in China. The StrataBox™ Marine Geophysical Instrument was applied for the first time to obtain high-resolution seismic data (in the form of vectorgraphs) of the lake sediment. Data were then interpreted by SonarWiz.Map acoustics software. Data were correlated with core stratigraphy from the lake as well as an outcrop on the northern side of the lake at Yao Bay. Results show that the upper 10 m sediment (beneath the interface of the sediment and the overlying lake water) is characterized by laminated sediments, which can be classified into two stratal types, i.e. lacustrine sediment stratum (U1) and underlying hard loess stratum (U2). The contact of these two lithologies is not continuous, and part of it is absent in the lake basin. Unequally spread over the lake basin, the lacustrine sediment (mainly consisting of sludge and muddy-clay) is found in areas along the western bank, to the northwest of the Xishan Mountains and along the northwestern side of the lake. In the rest of the lake basin, the hard loess stratum is exposed in outcrops. The depth of the lacustrine sediment ranges from 1 to 2 m, while the depth of the sludge (closely related to the modern lacustrine environment) varies from 0.03 to 1.0 m. The spatial distribution of lacustrine sediments in Taihu Lake is primarily influenced by transportation and sedimentation of riverine materials, as well as the hydrodynamics of lake currents.

Highlights

  • A geophysical survey was carried out for Taihu Lake, one of the largest shallow lakes in China

  • Our work provides valuable information regarding: 1) spatial distribution of the sediments in Taihu Lake; 2) accurate estimation of the load of inner contamination of the lake; and 3) feasibility of a proposal to dredge sludge from the lake in the near future

  • Notable is that deep water occurs along the water traffic areas, such as the shipping channel striking from the estuary of the Tiaoxi River to the estuary of the Wangyu River

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Summary

Introduction

A geophysical survey was carried out for Taihu Lake, one of the largest shallow lakes in China. To obtain accurate data on spatial distribution of sediments for the entire lake, we carried out a high-resolution geophysical survey on Taihu Lake over a period of more than four months. No. acquired seismic data (in the form of vectorgraphs) were interpreted in the lab by SonarWiz.Map acoustics software, to reveal reflection characteristics of the acoustic profiles of the sediments These were later correlated with stratigraphy of available sediment cores and previous geological surveys, and the stratigraphic sequences of our in situ drilled sediment cores, in order to obtain information on the spatial and temporal variations in stratigraphy of the sediments in Taihu Lake. Our work provides valuable information regarding: 1) spatial distribution of the sediments in Taihu Lake; 2) accurate estimation of the load of inner contamination of the lake; and 3) feasibility of a proposal to dredge sludge from the lake in the near future

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