农业环境科学学报
農業環境科學學報
농업배경과학학보
Journal of Agro-Environment Science
2010年
3期
546-550
,共5页
底泥%P滞留能力%太湖
底泥%P滯留能力%太湖
저니%P체류능력%태호
sediment%P retention%Taihu
磷(P)是湖泊富营养化的限制性营养元素,而沉积物是湖泊营养物质的重要蓄积库,沉积物对P的滞留能力是决定湖泊自净能力的重要因素.采用室内有机玻璃圆柱装置,研究了太湖两种污染程度不同的底泥对P的滞留能力.结果表明,污染程度较轻的黄泥在实验期间对P的最大滞留量为28.365 μmol·m~(-2),污染程度较重的黑泥最大滞留量仅为9.321μmol·m~(-2),两种底泥对P的滞留具有极显著的差异(P<0.01).与实验初期相比,实验末期黄泥中总磷增加0.06%,而在黑泥中却减少0.02%,黄泥对P的滞留能力远远大于黑泥.
燐(P)是湖泊富營養化的限製性營養元素,而沉積物是湖泊營養物質的重要蓄積庫,沉積物對P的滯留能力是決定湖泊自淨能力的重要因素.採用室內有機玻璃圓柱裝置,研究瞭太湖兩種汙染程度不同的底泥對P的滯留能力.結果錶明,汙染程度較輕的黃泥在實驗期間對P的最大滯留量為28.365 μmol·m~(-2),汙染程度較重的黑泥最大滯留量僅為9.321μmol·m~(-2),兩種底泥對P的滯留具有極顯著的差異(P<0.01).與實驗初期相比,實驗末期黃泥中總燐增加0.06%,而在黑泥中卻減少0.02%,黃泥對P的滯留能力遠遠大于黑泥.
린(P)시호박부영양화적한제성영양원소,이침적물시호박영양물질적중요축적고,침적물대P적체류능력시결정호박자정능력적중요인소.채용실내유궤파리원주장치,연구료태호량충오염정도불동적저니대P적체류능력.결과표명,오염정도교경적황니재실험기간대P적최대체류량위28.365 μmol·m~(-2),오염정도교중적흑니최대체류량부위9.321μmol·m~(-2),량충저니대P적체류구유겁현저적차이(P<0.01).여실험초기상비,실험말기황니중총린증가0.06%,이재흑니중각감소0.02%,황니대P적체류능력원원대우흑니.
Phosphoms(P)is a limited nutrient oflake eutrophication.Sediment is the important nutrient pool of lake ecosystems,and P re-tenfion capacity of sediment is an important factor determining the self-purification capacity of hkes.This paper studied the P retention ca-pacity of the sediments with different pollution(eutrophication)in Taihu.The results showed that the maximum P retention of yellow sediment with less poHution WaS 28.365 μmol·m~(-2),but that of black sediment with more pollution wag only 9.321 μmol·m~(-2).There was significant difference between the P retention capacity of two different sediments(ANOVAP<0.01).The TP of yellow sediment at the end of the ex-periment increased 0.06%,but that of black sediment decreased 0.02%.Our research indicated that the capacity of yellow sediment P reten-tion was far stronger than that of the black sediment.