湖北农业科学
湖北農業科學
호북농업과학
Hubei Agricultural Sciences
2015年
21期
5272-5276
,共5页
范廷玉%王月越%严家平%王顺%李国瑞%陈威
範廷玉%王月越%嚴傢平%王順%李國瑞%陳威
범정옥%왕월월%엄가평%왕순%리국서%진위
采煤沉陷区%浅层地下水%营养盐
採煤沉陷區%淺層地下水%營養鹽
채매침함구%천층지하수%영양염
coal mine subsidence area%shallow groundwater%nutrient
以淮南潘一、潘三矿采煤沉陷区(开放型沉陷区)和后湖采煤沉陷区(封闭型沉陷区)为研究区域,通过对沉陷区浅层地下水中氮、磷等营养盐指标的监测,研究了两种类型采煤沉陷积水区浅层地下水中营养元素的时空分布特征,采用相关性分析初步研究了不同类型沉陷区营养盐的迁移特征,同时分析了营养盐的限制性组成. 结果表明,NH3-N年内时间差异性较小,整体呈开放型浅层地下水(KD)>封闭型浅层地下水(FD);NO2--N、NO3--N和凯氏氮年内空间差异性较小,时间差异性较大,丰水期低于平枯水期;总氮年内时空差异性均较小,基本呈FD>KD.PO43-和总磷年内时间差异性较大,溶解性总磷年内时空差异性较小. 开放型沉陷区浅层地下水内各营养盐指标的相关性更强,封闭型沉陷区浅层地下水中磷的污染风险更大.
以淮南潘一、潘三礦採煤沉陷區(開放型沉陷區)和後湖採煤沉陷區(封閉型沉陷區)為研究區域,通過對沉陷區淺層地下水中氮、燐等營養鹽指標的鑑測,研究瞭兩種類型採煤沉陷積水區淺層地下水中營養元素的時空分佈特徵,採用相關性分析初步研究瞭不同類型沉陷區營養鹽的遷移特徵,同時分析瞭營養鹽的限製性組成. 結果錶明,NH3-N年內時間差異性較小,整體呈開放型淺層地下水(KD)>封閉型淺層地下水(FD);NO2--N、NO3--N和凱氏氮年內空間差異性較小,時間差異性較大,豐水期低于平枯水期;總氮年內時空差異性均較小,基本呈FD>KD.PO43-和總燐年內時間差異性較大,溶解性總燐年內時空差異性較小. 開放型沉陷區淺層地下水內各營養鹽指標的相關性更彊,封閉型沉陷區淺層地下水中燐的汙染風險更大.
이회남반일、반삼광채매침함구(개방형침함구)화후호채매침함구(봉폐형침함구)위연구구역,통과대침함구천층지하수중담、린등영양염지표적감측,연구료량충류형채매침함적수구천층지하수중영양원소적시공분포특정,채용상관성분석초보연구료불동류형침함구영양염적천이특정,동시분석료영양염적한제성조성. 결과표명,NH3-N년내시간차이성교소,정체정개방형천층지하수(KD)>봉폐형천층지하수(FD);NO2--N、NO3--N화개씨담년내공간차이성교소,시간차이성교대,봉수기저우평고수기;총담년내시공차이성균교소,기본정FD>KD.PO43-화총린년내시간차이성교대,용해성총린년내시공차이성교소. 개방형침함구천층지하수내각영양염지표적상관성경강,봉폐형침함구천층지하수중린적오염풍험경대.
To find out temporal and spatial distribution characteristics of nutrients such as nitrogen, phosphrous, etc in the shallow groundwater of different types of coal mine subsidence area, open (Pan1and Pan3) and closed (Houhu) subsidence area in Huainan were selected and nine sets of monitoring data from November 2012 to September 2013 were analyzed. Cor-relation analysis revealed different response relationship and migration characteristics of nitrogen and phosphorus in the same water body. Compositions of nitrogen and phosphorus in two types of water body were analyzed based on their ratios of vari-ous forms. Results showed that the temporal difference of NH3-N was small in both water bodies, though it was larger in KD (open shallow groundwater)than in FD (closed shallow groundwater) in general. On average, the temporal differences of NO2--N、NO3--N and KN were big, and the spatial differences were small, while both were lower during wet season than in dry or normal reason. The temporal and spatial distribution difference of total nitrogen (TN) were both little and presented FD>KD. The spatial difference of PO43- and TP was large, while the temporal and spatial difference of TSP was small. The nutrient elements were more related to each other in open subsidence area than in closed subsidence area as to the composi-tions of nitrogen and phosphorus, certain differences existed in the two water bodies and phosphorus pollution risk was greater in shallow underground water of closed coal mine subsidence area.