不同退水条件下典型圩区稻田-沟-塘系统氮磷浓度时空变化特征

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中图分类号X171文献标识码A

文章编号 0517-6611(2025)18-0063-08

doi:10.3969/j.issn.0517-6611.2025.18.015

SpatialandTemporal Variation CharacteristicsofNitrogenandPhosphorusConcentrationsinthePaddyField-Ditch-PondSystem ofPolderAreasUnderDifferentDrainageConditions

QIN Xian-yan,ZHENGTao(Geological SurveyotAnhui Province(Anhui InstituteofGeologicalSciences),Hetei,Anhui 2301) AbstractThespatialandtemporalvationsofnrogenandposporusconcentratiosintheaddfeld-dic-ondssteiinatypcal polderareaofteChaouLkeBasinereaalyzedusingfied-pointmonitoringResultsindicatedthatthetotalnitrogen(T)andaonm nitrogen ( NH4+ -N)concentrationsatninesampling points inthepaddyfielddrainageexhibitedsignificantspatialandtemporal heterogeneity during bothinlldgatiodageeventsHowevertoncentratiosaachsaplingntgenrallreasdasthooth periodprogrsedTeoncentrationinhowstreamtertarydichassigcantlyfluenedbyatofepadfielddragi highlysigniftositieoelatiosedetntoUnderotaaeodios,tratonateofospt tionwaslessdistnc.Insofpospousompositioarticulateposhos(P)wasthomnantforoftotalpospus(T)uder rainfall drainage,accounting for 69.28% to 85.43% ,whereasunder irigation drainage,the proportion of PP in TP was relatively lower ( 50.05% ).Ditchesatallevels withinthepolderarea demonstratedacertaincapacitytoretainTNandTP,withahigherretentioneiciency observedforTsefindinssuggesthateditcondstemspondeddierentlttrogenandposphousinpadfelddaigeunderrainfall and irrigation drainage conditions.

Keywordsddeld-dicodtefallaggatiodage;rgenndosporusoctratiosSpatialdt ral variation characteristics;Chaohu lake basin

圩田也称圩、皖或圩皖,一般是闭合的,通过节制闸或抽排水站进行圩内圩外水量交换,在抵御洪水中发挥了重要作用[1]。(剩余14664字)

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