周原全新世土壤剖面木炭屑与野火活动的关系研究

Relationship between soil charcoal in Holocene and wildfire in the Zhouyuan Region

  • 摘要: 研究陕西周原全新世黄土剖面磁化率曲线、总有机碳曲线、木炭屑曲线和野火活动及其与生态环境演变的关系结果表明,马兰黄土堆积时期气候干旱, 在当时半荒漠草原上当地时常有自然野火发生;全新世大暖时期(8500~3100aB.P)气候湿 润,生物成壤作用强度大,呈现森林或森林草原自然景观,野火活动极少发生;先周人迁 居到周原地区(3100aB.P)开始,人类用火及其放火烧荒开垦农田等活动,加之气候变得干 旱,生物化学成壤作用减弱,致使生态环境发生重大变化,自然生态景观向半自然、半人 工景观演替;1500aB.P开始可耕种土地几乎开垦殆尽,生态景观完全被人工农田生态景 观 所代替;而近几百年来随着人口密度和聚落的增加,人类生活用火和垃圾随之加大,人类 对土壤环境的干扰进一步增强。

     

    Abstract: The relationships among soil charcoal in Holocene,wildfire and its change of ecological environment were studied.The results show that in the phase of piling of Malan loess,the climate was arid and wildfire often occurred on semi-desert grassland.During the period of soil formation,bio-pedogenic processes were so active that forests or forest-grassland formed. However,by the time of 3100aB.P,with the settlement of Zhouyuan people and human manipulation of the environment through the use of the fire,great changes had taken place,varying from natural ecology to semi-natural and semi-artificial ecology.Since 1500aB.P,the arable farmland almost disappeared,resulting in artificial ecology in place of natural ecology.For hundreds of years,with the growth of the world population,tremendous requirements of fires had increased with a large amount production of rubbish and human activities had also caused great damage to the soil environment.

     

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