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梁子湖流域降雨径流过程及氮磷流失对不同景观格局的响应

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景观格局决定小流域能源流动与水沙过程,是影响氮磷流失的重要因素。以湖北梁子湖流域的双溪(农林复合型)和石桥(林地型)2个典型小流域为研究对象,在自然降雨条件下,于2016年1-12月对流域出口断面水质水量进行了连续监测,并结合丰水期典型次降雨径流过程,探讨了不同景观格局下小流域降雨径流过程和氮磷输出特征,为梁子湖环境综合治理提供一定的科学依据。结果表明:(1)降雨径流过程在不同景观格局小流域内呈现出明显差异。相比于双溪小流域,石桥小流域产流能力较强,径流过程呈现出汇流时间较短、径流响应速度较快、径流模数较大的趋势;(2)双溪小流域总氮(TN)和总磷(TP)月均输出浓度范围分别为1。29~4。28 mg/L和0。04~0。22 mg/L,均高于石桥小流域(TN:0。62~1。90 mg/L;TP:0。02~0。11 mg/L),其中硝态氮(NO3--N)是氮素流失的主要形态,占TN流失的51。8%~88。2%。相比于石桥小流域,双溪小流域的NO3--N/TN较大。2个小流域的氨氮(NH4+-N)和亚硝态氮(NO2--N)输出浓度均较低并且无明显变化趋势;(3)双溪小流域的TN和TP月均输出通量范围分别为1。83~20。03 g/s和0。04~1。45 g/s,均高于石桥小流域(TN:0。62~10。01 g/s;TP:0。01~0。54 g/s),且与同时段流量呈现显著正相关关系(P<0。01);(4)双溪小流域的TN和TP流失强度分别为3。68和0。20t/(km2·a),分别是石桥小流域的1。32倍和1。30倍。氮磷流失主要集中在降雨频繁的4-7月,占全年流失负荷的70%以上。综上,梁子湖流域景观格局显著影响养分流失,优化土地利用配置和科学合理施肥是改善该流域水环境的科学措施。
Responses of Rainfall-Runoff Processes and Nitrogen and Phosphorus Exports to Different Landscape Pattern in the Liangzi Lake Watershed
The landscape pattern controls the energy flow and water sediment process of the watershed,which is an impor-tant factor affecting nitrogen and phosphorus loss in small watershed.In order to understand the responses of rainfall-runoff processes and nitrogen and phosphorus exports to landscape pattern,two typical small watersheds,Shuangxi(agroforestry catchment)and Shiqiao(forest catchment)in the upper watershed of Liangzi Lake area of Hubei Province,were selected as the research objects.The water quality and quantity at the outlet of the watersheds were continuously monitored from Janu-ary to December and a secondary rainfall event in 2016.The results showed that the landscape patterns had a significant impact on responses of rainfall-runoff processes.Compared with Shuangxi,the runoff process in Shiqiao small watershed showed a trend of shorter convergence time,faster runoff response speed and larger runoff modulus.The monthly concentra-tions of total nitrogen(TN)and total phosphorus(TP)in Shuangxi small watershed were in the range of 1.29~4.28 mg/L and 0.04~0.22 mg/L,which were higher than those of Shiqiao(TN:0.62~1.90 mg/L;TP:0.02~0.11 mg/L),respectively.Nitrate nitrogen(NO3--N)was the major form of TN in the two small catchments,accounted for 51.8%~88.2%,but the proportion of NO3--N to TN in Shuangxi small watershed was higher than those of Shiqiao.The concentrations of ammonium(NH4+-N)and nitrite nitrogen(NO2--N)remained at a low level and exhibited no obvious trend.The emission fluxes of TN and TP in Shuangxi small watershed were in the range of 1.83~20.03 g/s and 0.04~1.45 g/s,which were higher than those of Shiqiao(TN:0.62~10.01 g/s;TP:0.01~0.54g/s),respectively.It was also found that there was a significant positive correlation between the TN and TP emission flux and runoff in the same period.The annual loss intensity of TN and TP in Shuangxi small watershed were 3.68 t/(km2·a)and 0.20 t/(km2·a),which were 1.32 and 1.30 times greater than those of Shiqiao,respec-tively.The losses of TN and TP in both small watersheds mainly occurred between April and July with frequent rainfall events,accounting for more than 70%of the annual total losses.In conclusion,different landscape patterns had a significant impact on the losses of TN and TP.Accordinglly,rational fertilization to reduce anthropogenic nitrogen and phosphorus loss and optimization of land use to store water and preserve soil are scientific measures to improve the water environment in the watershed.The study could provide more insights for reducing agricultural non-point source pollution in Liangzi Lake region and similar other regions.

rainfall-runoff processnitrogen and phosphorus lossesLiangzi Lakelandscape patternnon-point source pollution

王静、王峰、熊昱、杨雪、程益涵、吕国安、廖斌

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安徽省农业科学院土壤肥料研究所,养分循环与耕地保育安徽省重点实验室,安徽 合肥 230031

湖北省生态环境科学研究院(省生态环境工程评估中心),湖北 武汉 430072

长江水资源保护科学研究院,湖北 武汉 430051

湖北省水利水电规划勘测设计有限公司,湖北 武汉 430070

华中农业大学资源与环境学院,湖北 武汉 430070

武汉大学水利水电学院,湖北 武汉 430072

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径流过程 氮磷流失 梁子湖 景观格局 面源污染

安徽省重点研究与开发计划项目湖北省水利重点科研项目安徽省农业科学院院立科研项目国家青年科学基金项目

2022107020004HBSLKY2016012024YL00741401308

2024

环境科学与技术
湖北省环境科学研究院

环境科学与技术

CSTPCD北大核心
影响因子:0.943
ISSN:1003-6504
年,卷(期):2024.47(9)