通过毛乌素沙地现代风成砂与泊江海子剖面沉积物粒度特征对比分析,确定剖面中4个层位(290～210 cm,190～160 cm,153．5～123．5 cm,50～40 cm)基本属于风成砂沉积,这些风成砂中间夹杂着3次湖相沉积,结合年代序列认为此区域在5．8～4．5 ...通过毛乌素沙地现代风成砂与泊江海子剖面沉积物粒度特征对比分析,确定剖面中4个层位(290～210 cm,190～160 cm,153．5～123．5 cm,50～40 cm)基本属于风成砂沉积,这些风成砂中间夹杂着3次湖相沉积,结合年代序列认为此区域在5．8～4．5 cal kaBP存在以下沉积旋回:～5749 cal aBP沉积风成砂,反映该时期风砂活动强烈,气候干燥,冬季风强盛;5 749 cal aBP前后沉积物为灰绿色湖相层,表明这一时期存在短暂的湖面扩展,沙漠退缩;5 749～5370 cal aBP沉积风成砂,反映了湖泊的退缩和沙漠的扩展;5370～4895 cal aBP湖相沉积物,反映了流域降水量的增多;4895～4580 cal aBP沉积风成砂后,4580 cal aBP前后又出现了短暂的湖相沉积,之后又是风砂沉积．展开更多
The water characteristic curve for aeolian sand in two processes of wetting and drying was obtained by the negative water column technique.The values of fitting parameters were calculated according to Van Genuchten fo...The water characteristic curve for aeolian sand in two processes of wetting and drying was obtained by the negative water column technique.The values of fitting parameters were calculated according to Van Genuchten formula and the parameters that characterized the prosperities of aeolian sand such as the unsaturated infiltration coefficient and specific water capacity were obtained.The results showed that the water characteristic curve for aeolian sand in wetting process had greater hysteresis quality than ...展开更多
文摘通过毛乌素沙地现代风成砂与泊江海子剖面沉积物粒度特征对比分析,确定剖面中4个层位(290～210 cm,190～160 cm,153．5～123．5 cm,50～40 cm)基本属于风成砂沉积,这些风成砂中间夹杂着3次湖相沉积,结合年代序列认为此区域在5．8～4．5 cal kaBP存在以下沉积旋回:～5749 cal aBP沉积风成砂,反映该时期风砂活动强烈,气候干燥,冬季风强盛;5 749 cal aBP前后沉积物为灰绿色湖相层,表明这一时期存在短暂的湖面扩展,沙漠退缩;5 749～5370 cal aBP沉积风成砂,反映了湖泊的退缩和沙漠的扩展;5370～4895 cal aBP湖相沉积物,反映了流域降水量的增多;4895～4580 cal aBP沉积风成砂后,4580 cal aBP前后又出现了短暂的湖相沉积,之后又是风砂沉积．
基金Supported by Key Project of Science and Technology Research of Ministry of Education(308021)Chang Jiang Scholars Innovation Team of Ministry of Education(IRT0811)Geological Survey Project of China Geological Survey(1212010331302)~~
文摘The water characteristic curve for aeolian sand in two processes of wetting and drying was obtained by the negative water column technique.The values of fitting parameters were calculated according to Van Genuchten formula and the parameters that characterized the prosperities of aeolian sand such as the unsaturated infiltration coefficient and specific water capacity were obtained.The results showed that the water characteristic curve for aeolian sand in wetting process had greater hysteresis quality than ...
