中国环境科学
中國環境科學
중국배경과학
CHINA ENVIRONMENTAL SCIENCE
2014年
6期
1548-1555
,共8页
王书航%姜霞%王雯雯%胡佳晨%张博%李佳璐%赵丽
王書航%薑霞%王雯雯%鬍佳晨%張博%李佳璐%趙麗
왕서항%강하%왕문문%호가신%장박%리가로%조려
蠡湖%悬浮物%时空分布%影响因素%治理措施
蠡湖%懸浮物%時空分佈%影響因素%治理措施
려호%현부물%시공분포%영향인소%치리조시
Lihu Lake%suspended matter%spatial-temporal distributions%influencing factor%treatment measure
根据2012~2013年的现场调查资料和历史监测资料,分析了浅水湖泊蠡湖总悬浮物(TSS)的时空分布特征、组成、变化规律,并探讨了水体悬浮物的影响因素及其与氮、磷的关系.结果表明,ρ(TSS)的年内变化范围在1.00~78.00mg/L之间,平均值为17.35mg/L,空间上呈现东蠡湖大于西蠡湖,沿岸高于湖心区的分布趋势;季节变化表现为秋季>夏季>春季>冬季,且冬季显著低于其他季节;全湖水体中ρ(OSS)和ρ(ISS)所占ρ(TSS)的比例相当,分别为51.52%和48.48%,但组成比例空间差异较大,东蠡湖ρ(OSS)比例较大,而西蠡湖ρ(ISS)的比例较大.线性拟合表明,ρ(TSS)与ρ(PN)、ρ(TN)、ρ(PP)、ρ(TP)均具呈显著正相关(P<0.01).浮游藻类增殖、水生植物的残体以及底泥的再悬浮是影响水体ρ(TSS)的主要因素.
根據2012~2013年的現場調查資料和歷史鑑測資料,分析瞭淺水湖泊蠡湖總懸浮物(TSS)的時空分佈特徵、組成、變化規律,併探討瞭水體懸浮物的影響因素及其與氮、燐的關繫.結果錶明,ρ(TSS)的年內變化範圍在1.00~78.00mg/L之間,平均值為17.35mg/L,空間上呈現東蠡湖大于西蠡湖,沿岸高于湖心區的分佈趨勢;季節變化錶現為鞦季>夏季>春季>鼕季,且鼕季顯著低于其他季節;全湖水體中ρ(OSS)和ρ(ISS)所佔ρ(TSS)的比例相噹,分彆為51.52%和48.48%,但組成比例空間差異較大,東蠡湖ρ(OSS)比例較大,而西蠡湖ρ(ISS)的比例較大.線性擬閤錶明,ρ(TSS)與ρ(PN)、ρ(TN)、ρ(PP)、ρ(TP)均具呈顯著正相關(P<0.01).浮遊藻類增殖、水生植物的殘體以及底泥的再懸浮是影響水體ρ(TSS)的主要因素.
근거2012~2013년적현장조사자료화역사감측자료,분석료천수호박려호총현부물(TSS)적시공분포특정、조성、변화규률,병탐토료수체현부물적영향인소급기여담、린적관계.결과표명,ρ(TSS)적년내변화범위재1.00~78.00mg/L지간,평균치위17.35mg/L,공간상정현동려호대우서려호,연안고우호심구적분포추세;계절변화표현위추계>하계>춘계>동계,차동계현저저우기타계절;전호수체중ρ(OSS)화ρ(ISS)소점ρ(TSS)적비례상당,분별위51.52%화48.48%,단조성비례공간차이교대,동려호ρ(OSS)비례교대,이서려호ρ(ISS)적비례교대.선성의합표명,ρ(TSS)여ρ(PN)、ρ(TN)、ρ(PP)、ρ(TP)균구정현저정상관(P<0.01).부유조류증식、수생식물적잔체이급저니적재현부시영향수체ρ(TSS)적주요인소.
The spatial-temporal distribution characteristics, composition and change rule of ρ(TSS) in Lihu Lake, a shallow lake, were analyzed by field survey data and historical monitoring data in 2012~2013. The key impacting factors ofρ(TSS) and relationship between it and nitrogen, phosphorus were discussed. Results showed that the annualρ(TSS) was 1.00~78.00mg/L, with the mean value of 17.35mg/L.ρ(TSS) in east Lihu Lake and coastal areas was higher than that in west Lihu Lake and lake center, respectively. The seasonal characteristics of ρ(TSS) was autumn>summer>spring>winter, andρ(TSS) in winter was significantly lower than the other seasons.ρ(OSS) andρ(ISS) almost took the same proportion ofρ(TSS) in the whole lake, with the value of 51.52%and 48.48%, respectively. While significant spatial heterogeneity existed in the composition ratio. OSS was the main composition of east Lihu Lake, but the suspended matter of west Lihu Lake mainly existed in inorganic component. Results of multivariate regression analysis showed thatρ(TSS) was significant positive correlated withρ(PN),ρ(TN),ρ(PP), andρ(TP) (P<0.01). Planktonic algae proliferation, residues of aquatic plants and sediment resuspension were the main factors influencingρ(TSS) in water.