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中国农学通报 ›› 2018, Vol. 34 ›› Issue (7): 85-89.doi: 10.11924/j.issn.1000-6850.casb17100057

所属专题: 园艺

• 资源 环境 生态 土壤 气象 • 上一篇    下一篇

南方山地茶园小流域径流演变规律

刘岑薇,张燕,陈锦辉,杨冬雪,王义祥   

  1. 福建省农业科学院农业生态研究所,福建省环境监测中心站,福建省环境监测中心站,福建省环境监测中心站,福建省农业科学院农业生态研究所
  • 收稿日期:2017-10-17 修回日期:2018-02-01 接受日期:2018-01-02 出版日期:2018-03-07 发布日期:2018-03-07
  • 通讯作者: 刘岑薇
  • 基金资助:
    福建省公益类科研院所专项“组合指纹法在山地茶园侵蚀小流域产沙来源的应用”(2016R1016-4);福建省农业科学院青年人才创新基金 “茶园集中开发区泥沙来源及其迁移规律研究”(2015QC-5)。

Evolvement Rule of Small Watershed Runoff in Hillslope Tea Garden in Southern Area

  • Received:2017-10-17 Revised:2018-02-01 Accepted:2018-01-02 Online:2018-03-07 Published:2018-03-07

摘要: 以分析南方山地茶园小流域降雨对径流的变化规律,为南方小流域水资源可持续高效利用提供理论依据。本研究在福建省安溪县山地茶园小流域的出口设置卡口站,连续3 年(2014—2016 年)对该区域降雨量、径流以及对卡口站中泥沙量进行监测,且对泥沙颗粒组分进行分析。结果表明:该区域受气温影响,降雨多集中在7、8 月,径流受到降雨及气候影响,导致径流的补给年内分配差异较大。随着土壤由湿润到水分饱和,入渗量逐渐减小,径流量增大,雨水对地表的冲刷能力增强,径流量由小变大使得大颗粒泥沙被冲刷。另外,在卡口站入口处的颗粒分布从上层到下层呈增大的趋势。该区域降水逐年递增,径流量主要受到气候的变化,随降水量增大而增大。随着人类活动的增大,对该区域径流量也有一定的影响。

Abstract: The effect of precipitation on runoff in hillslope tea garden in southern area was analyzed to provide a theoretical basis for sustainable and efficient utilization of water resources. The seasonal and annual variation characteristics of precipitation and runoff- yield in tea garden in Anxi of Fujian were analyzed based on hydrological data during 2014-2016. Sediment grain size distribution in water station was analyzed as well. The results showed that: the region was affected by the temperature, and precipitation was concentrated in July and August. Runoff was affected by precipitation and climate resulting in greater distribution differences of runoff during the year; with the soil from wetting to water saturation, the infiltration amount was gradually reduced, and the runoff volume was increased. Scour ability of rainwater to the surface was increased, so that runoff was changed from small amount to large amount, which caused the transportation of large grain sediment. In addition, sediment grain size distribution increased from upper layer to lower layer at the entrance years, increase of human activities also has certain influence on runoff.

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