首页|多因素视角下喀斯特地貌土地利用对河流水质的响应关系:以赤水河流域(云南段)为例

多因素视角下喀斯特地貌土地利用对河流水质的响应关系:以赤水河流域(云南段)为例

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为探究不同空间尺度、季节和地形坡度等多因素视角下喀斯特地貌土地利用与河流水质的响应关系,根据滇东北典型喀斯特地貌赤水河流域(云南段)2021年丰、平、枯水期TN、TP浓度监测数据,结合土地利用类型及坡度遥感监测影像,基于200 m缓冲区、500m缓冲区、1000m缓冲区和子流域4种空间尺度定量描述了赤水河(云南段)水质对流域土地利用的响应关系。结果表明:(1)赤水河流域(云南段)2021年Ⅰ~Ⅲ类水质占总体的87。0%,水环境质量总体良好,但TN超标较为严重,部分断面超标可达4倍以上;(2)随空间尺度增大,林地与TN正相关性增强,子流域尺度下相关性显著(0。720,P<0。05)。多元线性回归R2拟合结果表明,子流域尺度对水质变化的解释度最高;(3)丰水期陡坡(坡度>25°)林地与TP呈显著正相关(0。795,P<0。05),平水期、枯水期与TN呈显著正相关(依次为0。728,P<0。05;0。800,P<0。01);丰水期缓坡(坡度8°~25°)建设用地与TN呈显著正相关(0。733,P<0。05)。显著相关性主要集中于缓坡及陡坡地带;(4)林地、牧场、耕地是水质变化的主要影响因子。其中,牧场在流域面积中占比最小,却能够对河流水质产生较大影响,因此,对牧场进行管理能够以较高效率改善河流水质。研究结果可为喀斯特地貌土地利用对河流水质的响应研究提供理论依据。
Response Relationship of Land Use in Karst Landscapes to River Water Quality in a Multifactorial Perspective:a Case Study of Chishui River Basin
The objective of this paper is to probe into the relationship between land use and river water quality in karst landscapes in terms of varied spatial scales,seasons,and topographic slopes.On the basis of the river-water monitoring data of TN and TP concentrations of of the Chishui River(Yunnan Section)in 2021 within the typical karst geomorphologic basin of northeast Yunnan Province in combination with remote sensing images of the types of land-use and slope,quantitative description about the response of water quality to land-use in the watershed was made according to four spatial scales:200 m buffer zone,500 m buffer,1 000 m buffer zone,as well as the sub-watershed.Results showed the water quality of the river-water of Chishui River Basin(Yunnan Section)in 2021 ranged between categories Ⅰ and Ⅲ,accounting for 87.0%of the total;so generally the quality of the water environment was good,except for TN concentration,which exceeded the the relevant state standard by more than four times in some sections.Owing to the enhancement of spatial scale and the posi-tive correlation between forest-land and TN,the correlation in the lower sub-watersheds scale was significant(0.720,P<0.05),and the multiple linear regression R-square fitting results showed that the sub-basin scale has the highest degree of explanation for water quality changes;steep-slope forest land was positively correlated with TP during the wet season(0.795,P<0.05),with TN during the level period(0.728,P<0.05),and with the dry season(0.800,P<0.01);while the gen-tle-slope land for construction was significantly in positive correlation with TN during the wet season(0.733,P<0.05);these significant correlations were mainly located in the areas with gentle-slope and steep-slope;and forest land,pasture-land,and farmland were the main factors affecting the change of water quality;however among others,pastureland though accounting for the smallest proportion of the watershed area,it had a considerable impact on the river water quality.There-fore,the adequate management of pastureland could improve the river water quality with higher efficiency.It is expected that the research achievements could provide a theoretical basis for studying the impacts of land use on river water quality in the area of karst landscape.

nitrogen and phosphorus pollutionterrain slopeland usekarst landscape

范佳乐、李玥葶、程明豪、张亘、高欣、顾济沧、朱彬、宁平、黄建洪

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昆明理工大学环境科学与工程学院,云南 昆明 650500

云南省水文水资源局昆明分局,云南 昆明 650106

云南省生态环境对外合作中心,云南 昆明 650034

云南省生态环境监测中心,云南 昆明 650034

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氮磷污染 地形坡度 土地利用 喀斯特地貌

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(12)