首页> 外文期刊>Transactions of the ASAE >THE LONG–TERM FIELD–SCALE HYDROLOGY OF SUBSURFACE DRAINAGE SYSTEMS IN A COLD CLIMATE
【24h】

THE LONG–TERM FIELD–SCALE HYDROLOGY OF SUBSURFACE DRAINAGE SYSTEMS IN A COLD CLIMATE

机译:寒冷气候下地下排水系统的长期田间尺度水文

获取原文
获取原文并翻译 | 示例
           

摘要

Subsurface drainage is a common practice in the agricultural regions of the northern Midwest. Concerns about the impact of subsurface drainage on surface water quality and hydrology have increased over the past decade, spawning continued research on artificial drainage. Annual and decadal climatic variability necessitates a long-term perspective to fully evaluate these impacts. In addition, less is known about the hydrology of artificially drained lands in cold regions, where soil freezing and snowmelt routinely occur. A field-scale hydrologic analysis of subsurface drainage was performed using DRAINMOD v5.1 for an 85-year climatic period (1915 to 1999) for south-central Minnesota. This version of DRAINMOD included modifications for soil freeze/thaw and snowmelt processes. The results give insight into the long-term variations of subsurface drainage and other precipitation abstractions in a cold climate. Seasonal hydrology was characterized by well defined drainage and evapotranspiration (ET) "seasons" from March to June and from July to October, respectively. On average, 74% of infiltrated water was removed by subsurface drainage during the drainage season (March to June), representing 27% of annual precipitation. Significant increases in the 28-year average precipitation and drainage depths were apparent over the 85-year simulation period. Frequency and extreme value analysis revealed that annual drainage represented approximately 40% of annual precipitation at the 2-year return interval. Simulated annual drainage volumes were distributed normally, wherein the predicted 100-year annual drainage depth was 532 mm. Decreased drain spacing was found to significantly affect infiltration and drainage over the 85-year period. The results have potential uses for drainage practitioners, water management decision makers, and environmental and agricultural scientists and may pose significant challenges for addressing water quality issues on artificially drained lands
机译:在中西部北部的农业地区,地下排水是一种普遍做法。在过去的十年中,人们对地下排水对地表水质量和水文学的影响的担忧增加,催生了对人工排水的持续研究。年度和年代际气候变化需要长期的观点来全面评估这些影响。另外,对于寒冷地区的人工流失土地的水文学知之甚少,那里经常发生土壤冻结和融雪。使用DRAINMOD v5.1对明尼苏达州中南部的85年气候时期(1915年至1999年)进行了田间规模的地下排水水文分析。此版本的DRAINMOD包括对土壤冻结/融化和融雪过程的修改。结果为洞悉寒冷气候下地下排水和其他降水抽象的长期变化提供了见识。季节性水文学的特征是分别在3月至6月和7月至10月的明确的排水和蒸散(ET)“季节”。平均而言,在排水季节(3月至6月),地下排水除去了74%的渗入水,占年降水量的27%。在85年的模拟期内,平均28年的平均降水和排水深度明显增加。频率和极值分析表明,在2年的回归间隔内,年排水量约占年降水量的40%。模拟的年排水量呈正态分布,其中预测的100年年排水深度为532 mm。发现排水间距的减小在85年的时间内显着影响了渗透和排水。该结果对于排水从业人员,水管理决策者以及环境和农业科学家具有潜在的用途,并且可能在解决人工流失土地上的水质问题方面面临重大挑战

著录项

  • 来源
    《Transactions of the ASAE》 |2003年第4期|p.1011-1021|共11页
  • 作者

    C.-X. Jin; G. R. Sands;

  • 作者单位

    Chang-Xing Jin, Research Associate , and Gary R. Sands, ASAE Member Engineer, Assistant Professor;

    Department of Biosystems and Agricultural Engineering, University of Minnesota, St. Paul, Minnesota. Corresponding author: Gary R. Sands, University of Minnesota, 1390 Eckles Avenue, St. Paul, MN 55108;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    DRAINMOD; Hydrology; Long-term simulation; Subsurface drainage;

    机译:DRAINMOD;水文学;长期模拟;地下排水;

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号