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OALib Journal期刊
ISSN: 2333-9721
费用：99美元
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汉江上游谷地全新世风成黄土及其成壤改造特征
DOI: 10.11821/xb201111012, PP. 1562-1573
Keywords: 沙尘暴堆积物,成壤改造,全新世,汉江上游谷地
Abstract:
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(11500aBP),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(11500-8500aBP),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(8500-3000aBP),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(3000aBP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。
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