新疆大学绿洲生态教育部重点实验室
纸质出版:2014
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[1]夏倩倩,马家驹,张峰.塔克拉玛干沙漠腹地克里雅河尾闾圆沙三角洲沙质沉积物粒度特征[J].新疆大学学报(自然科学版),2014,31(01):12-16+127.
夏倩倩, 马家驹, 张峰. 塔克拉玛干沙漠腹地克里雅河尾闾圆沙三角洲沙质沉积物粒度特征[J]. Journal of Xinjiang University (Natural Science Edition in Chinese and English), 2014, 31(1): 12-16.
测定计算了圆沙古城遗址一带33个沙丘沙和36个剖面沙样品的粒度参数
总样品平均粒径变化于1.19-4.07Φ之间
均值3.21Φ
平均粒径2~3Φ间样品占总数的17%
3~4Φ间样品占总数的77%.其中沙丘沙平均粒径为2.96Φ
标准偏差范围在0.27~1.60Φ之间
偏度由极负偏至极正偏(-0.77~1)
峰度值介于0.45~1.83之间
剖面沙平均粒径3.43Φ
标准偏差在0.16~1.47Φ之间
偏度由极负偏至正偏(-0.78~0.12)
峰度值介于0.67~6.29.认为该研究区沙物质组成以极细沙为主
细沙为次;沙丘沙以受风力影响为主
而剖面沉积物则多受水力作用.与前人研究的塔克拉玛干沙漠南缘和北缘的粒度特征进行比较发现
三个地区沙物质粒度特征存在差别
反映了沙物质来源和沉积环境的不同.
33 dune sands and 36 section sand samples from 18 sections around Yuansha Site were collected and their grain size parameters were measured and calculated.the average particle diameter of all the samples are between 1.19-4.07 Φ with a mean value of 3.21 Φ
the samples with the average particle size of 2-3 Φ add up to 17%
while those between 3-4 Φ accounted for 77%.The sand dune mean grain size values
standard deviation value
skewness value and kurtosis value were of 2.96
0.27-1.60
-0.77-1 and 0.45-1.83 respectively
while those parameters of section samples were of 3.43
0.16-1.47
-0.78-0.12
0.67-6.29 correspondingly.Our measurement show most sediment samples can be classified into fine sand and the silver.For the formation cause
dunes samples are mainly affected by wind
sections samples are by water.Compared our measured grain size characteristics measurements with previous published work at the north as well as the south of the Taklimakan Desert
there are differences
which distinctly indicate the material source origination and the sediment mixture and sorting process discrepancy of inner Taklimakan desert.
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