地理学报 ›› 2011, Vol. 66 ›› Issue (11): 1562-1573.doi: 10.11821/xb201111012
庞奖励, 黄春长, 周亚利, 查小春, 王朝建
收稿日期:
2011-06-13
修回日期:
2011-09-09
出版日期:
2011-11-20
发布日期:
2011-11-20
作者简介:
庞奖励(1963-), 男, 西安市人, 博士, 教授, 中国地理学会会员(S110005769M), 主要从事土地利用与土壤演变的研究。E-mail: jlpang@snnu.edu.cn
基金资助:
国家自然科学重点基金项目(41030637);国家社会科学基金重点项目(11AZS009)
PANG Jiangli, HUANG Chunchang, ZHOU Yali, ZHA Xiaochun, WANG Chaojian
Received:
2011-06-13
Revised:
2011-09-09
Online:
2011-11-20
Published:
2011-11-20
Supported by:
NationalNatural Science Foundation of China, No.41030637; National Social Science Foundation of China, N0.11AZS009
摘要: 对汉江上游郧县—郧西段一级阶地物质上堆积的黄土状覆盖层的剖面构型、粒度、矿物组合、元素分布、微形态及形成时代进行了研究,并与渭河谷地全新世黄土—古土壤序列对比。结果表明,这些“黄土状覆盖层”是晚更新世以来沙尘暴在区内连续堆积的结果,具有TS-L0-S0-Lt-L1-AD剖面构型;这些风积物在不同时期受到了不同程度的成壤改造作用,晚更新世受到弱成壤改造→全新世中期受到强烈成壤改造→全新世晚期较弱成壤改造。汉江上游地区在晚更新世末期(11500 a BP),气候比较冷湿,沙尘暴频繁出现,形成较厚的黄土层L1;全新世初期(11500-8500 a BP),气候从冷湿向暖湿方向转变,沙尘暴活动减弱,形成了过渡黄土层位Lt;全新世中期(8500-3000 a BP),气候达到全新世最为暖湿的阶段,沙尘暴沉积物受到强烈成壤改造而形成了古土壤S0;全新世晚期(3000 a BP以来),气候暖湿程度降低,越过秦岭的沙尘暴又明显增强,形成了近代黄土L0。
庞奖励, 黄春长, 周亚利, 查小春, 王朝建. 汉江上游谷地全新世风成黄土及其成壤改造特征[J]. 地理学报, 2011, 66(11): 1562-1573.
PANG Jiangli, HUANG Chunchang, ZHOU Yali, ZHA Xiaochun, WANG Chaojian. Holocene Aeolian Loess and Its Pedogenic Modification in the Upper Hanjiang River Valley, China[J]. Acta Geographica Sinica, 2011, 66(11): 1562-1573.
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