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祁连山中段新冰期以来的冰川序列及环境变化

The stage-division and environmental significance of moraine in Qiyi glacier, Qilian Shan

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【作者】 杨威周尚哲CHIYUKI Narama王孝理王杰

【Author】 YANG Wei,ZHOU Shang-zhe,CHIYUKI Narama,WANG Xiao-li,WANG Jie (School of Resources and Environmental Sciences, Lanzhou University, Lanzhou 730000, China; Department of Geography, South China Normal University, Guangzhou 510080, China; Department of Environmental Studies, Nagoya University, Nagoya 494-8601, Japan)

【机构】 兰州大学资源环境学院华南师范大学地理系 广东 广州 510080名古屋大学地球水循环研究所甘肃 兰州 730000日本 名古屋 464-8601

【摘要】 通过对七一冰川及其附近冰碛垅形态、植被覆盖、岩石种类及Schmidt hammer反弹R值、剖面内部组成的观测、对比和分析,认为新冰期时冰川扩张到海拔4 km处,较现代冰川末端降低约300 m,冰川前进约2 km左右.小冰期的三列冰碛垅形成时间间隔基本相同,规模依次减小,表明小冰期的三次冷期中以15世纪最冷,持续时间最长,而17世纪次之,19世纪持续时间最短.

【Abstract】 The observations and comparisons of the features of debris, lichens, vegetation, soil weathering and R-values of Schmidt hammer indicate that the 7.1 glacier had advanced about 2 km and reached 4 km in the Neoglaciation. During the little ice age, three end moraines were formed in sequence, which demonstrates that the temperature in the 15th century was lowest and might have lasted a much longer time in little ice age. Moreover, the temperature in the 17th century was colder than that in the 19th century.

【关键词】 七一冰川冰碛垅小冰期
【Key words】 Qiyi glaciermoraine successionslittle ice age
【基金】 国家自然科学基金资助项目(40371013)
  • 【文献出处】 兰州大学学报 ,Journal of Lanzhou University , 编辑部邮箱 ,2006年06期
  • 【分类号】P534.63
  • 【被引频次】14
  • 【下载频次】332
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