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不同雨强下黄棕壤坡耕地径流养分输出机制研究
  • ISSN号:0250-3301
  • 期刊名称:《环境科学》
  • 时间:0
  • 分类:X52[环境科学与工程—环境工程]
  • 作者机构:[1]三峡大学水利与环境学院,三峡库区生态环境教育部工程研究中心,宜昌443002, [2]湖北工业大学资源与环境学院,武汉430072
  • 相关基金:国家自然科学基金项目(51179095,51179205),国家自然科学基金青年基金项目(51009080,51009081,51209123); 国家杰出青年科学基金项目(50925932); 三峡大学研究生科研创新基金项目(2011CX009); 水利部公益性行业科研专项(201201030); 三峡大学人才科研启动基金项目(KJ2012B038)
中文摘要:

为揭示三峡库区坡耕地在不同雨强下氮、磷养分随地表径流和壤中流的输出规律,在香溪河流域选择具有代表性的黄棕壤坡耕地进行原位人工模拟降雨试验.结果表明,在降雨总量一定的情况下,随雨强的增大,地表径流量、径流总量、泥沙侵蚀量均呈明显的增加趋势,而壤中流流量减少.不同雨强下地表径流中TN、DN、DP均存在明显的初期径流冲刷效应,TP在整个降雨过程中波动较大,呈微弱降低的变化趋势;壤中流中TN、DN、DP随降雨持续输出浓度无明显变化,TP在径流初期出现浓度峰值,之后减少并趋于稳定.雨强对磷素的影响更直接,雨强越大,磷素径流浓度也越大,氮、磷养分的平均浓度均远超出水体富营养化阈值.随雨强的增大,TN径流流失量减小,TP流失量增大,TN随地表径流流失贡献率随雨强的增大由36.5%增加至57.6%,磷素以地表径流为主,贡献率达90.0%以上,因此,控氮关键是减少壤中流的产生,控磷则需防止土壤侵蚀.随雨强的减小,地表径流中以溶解态流失的氮素比例升高,壤中流中均以溶解态为主,磷素的流失在不同雨强和径流形式下均以颗粒态为主.

英文摘要:

In order to investigate the loss characteristics of N and P through surface flow and interflow under different rainfall intensities,a field experiment was conducted on the sloping arable land covered by typical yellow-brown soils inXiangxi River watershed by artificial rainfall.The results showed that the discharge of surface flow,total runoff and sediment increased with the increase of rain intensity,while the interflow was negatively correlated with rain intensity under the same total rainfall.TN,DN and DP were all flushed at the very beginning in surface flow underdifferent rainfall intensities;TP fluctuated and kept consistent in surface flow without obvious downtrend.While TN,DN and DP in interflow kept relatively stable in the whole runoff process,TP was high at the early stage,then rapidly decreased with time and kept steady finally.P was directly influenced by rainfall intensity,its concentration in the runoff increased with the increase of the rainfall intensity,the average concentration of N and P both exceeded the threshold of eutrophication of freshwater.The higher the amount of P loss was,the higher the rain intensity.The change of N loss was the opposite.The contribution rate of TN loss carried by surface flow increased from 36.5% to 57.6% with the increase of rainfall intensity,but surface flow was the primary form of P loss which contributed above 90.0%.Thus,it is crucial to control interflow in order to reduce N loss.In addition,measures should be taken to effectively manage soil erosion to mitigate P loss.The proportion of dissolved nitrogen in surface flow elevated with the decrease of rainfall intensity,but in interflow,dissolved form was predominant.P was exported mainly in the form of particulate under different rainfall intensities and runoff conditions.

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期刊信息
  • 《环境科学》
  • 中国科技核心期刊
  • 主管单位:中国科学院
  • 主办单位:中国科学院生态环境研究中心
  • 主编:赵进才
  • 地址:北京市2871信箱(海淀区双清路18号)
  • 邮编:100085
  • 邮箱:hjkx@rcees.ac.cn
  • 电话:010-62941102 62849343
  • 国际标准刊号:ISSN:0250-3301
  • 国内统一刊号:ISSN:11-1895/X
  • 邮发代号:2-821
  • 获奖情况:
  • 在全国第一届和第二届优秀科技期刊评比中分别荣获...,二次荣获中国科学院优秀期刊评比一等奖,荣获中国期刊方阵双奖期刊荣誉
  • 国内外数据库收录:
  • 俄罗斯文摘杂志,美国化学文摘(网络版),荷兰文摘与引文数据库,美国工程索引,美国生物医学检索系统,美国剑桥科学文摘,美国生物科学数据库,英国动物学记录,日本日本科学技术振兴机构数据库,中国中国科技核心期刊,中国北大核心期刊(2004版),中国北大核心期刊(2008版),中国北大核心期刊(2011版),中国北大核心期刊(2014版),中国北大核心期刊(2000版)
  • 被引量:69962