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XUE Ji-bing. Variations in Dust Event Reflected by Grainsize Component of Lacustrine  Records in Droughty Area:a case study on Barkol Lake, Xinjiang, China[J]. Acta Sedimentologica Sinica, 2008, 26(4): 647-654.
Citation: XUE Ji-bing. Variations in Dust Event Reflected by Grainsize Component of Lacustrine  Records in Droughty Area:a case study on Barkol Lake, Xinjiang, China[J]. Acta Sedimentologica Sinica, 2008, 26(4): 647-654.

Variations in Dust Event Reflected by Grainsize Component of Lacustrine  Records in Droughty Area:a case study on Barkol Lake, Xinjiang, China

  • Received Date: 1900-01-01
  • Rev Recd Date: 1900-01-01
  • Publish Date: 2008-08-10
  • Grainsize analysis of BLK1 section, retrieved from Barkol Lake, NW China, was carried out using a Malvern 2000 grainsize analyzer, and environmentally sensitive grainsize components can be easily identified according to the variations in the grainsize standard deviation. The results indicated that 45~170 μm grainsize component and its mean grainsize diameter are sensitive to the regional dust events in the study area, combined with the radiocarbon ages, the dust events during the last 9.4 cal ka BP was reconstructed.
    During the last 2 000 years, strong dust events appeared at 240~440 cal aBP, 600~1 280 cal aBP and 1 400~1 800 cal aBP epochs, which are consistent well with the high values of raindust frequency and high contents of ions in Guliya Ice Core. During the last 9.4 cal kaBP, 8 000~8 300 cal aBP, 7 400~77 00 cal aBP, 6 500~7 000 cal aBP, especially during the middle Holocene epoch of 3 900~6 100 cal aBP, the regional dust events took place continually, which can contrast well with the microparticulate records in Guliya and Dunde Ice Cores. Lacustrine sediment in droughty areas is a good carrier which can denote the dust events during the historical period well, as the climatic variations has great regional characteristics, and so the environmentally sensitive grainsize components in some one section could not be used universally.
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    沈阳化工大学材料科学与工程学院 沈阳 110142

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  • Received:  1900-01-01
  • Revised:  1900-01-01
  • Published:  2008-08-10

Variations in Dust Event Reflected by Grainsize Component of Lacustrine  Records in Droughty Area:a case study on Barkol Lake, Xinjiang, China

Abstract: Grainsize analysis of BLK1 section, retrieved from Barkol Lake, NW China, was carried out using a Malvern 2000 grainsize analyzer, and environmentally sensitive grainsize components can be easily identified according to the variations in the grainsize standard deviation. The results indicated that 45~170 μm grainsize component and its mean grainsize diameter are sensitive to the regional dust events in the study area, combined with the radiocarbon ages, the dust events during the last 9.4 cal ka BP was reconstructed.
During the last 2 000 years, strong dust events appeared at 240~440 cal aBP, 600~1 280 cal aBP and 1 400~1 800 cal aBP epochs, which are consistent well with the high values of raindust frequency and high contents of ions in Guliya Ice Core. During the last 9.4 cal kaBP, 8 000~8 300 cal aBP, 7 400~77 00 cal aBP, 6 500~7 000 cal aBP, especially during the middle Holocene epoch of 3 900~6 100 cal aBP, the regional dust events took place continually, which can contrast well with the microparticulate records in Guliya and Dunde Ice Cores. Lacustrine sediment in droughty areas is a good carrier which can denote the dust events during the historical period well, as the climatic variations has great regional characteristics, and so the environmentally sensitive grainsize components in some one section could not be used universally.

XUE Ji-bing. Variations in Dust Event Reflected by Grainsize Component of Lacustrine  Records in Droughty Area:a case study on Barkol Lake, Xinjiang, China[J]. Acta Sedimentologica Sinica, 2008, 26(4): 647-654.
Citation: XUE Ji-bing. Variations in Dust Event Reflected by Grainsize Component of Lacustrine  Records in Droughty Area:a case study on Barkol Lake, Xinjiang, China[J]. Acta Sedimentologica Sinica, 2008, 26(4): 647-654.

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