Spatial distribution of phosphorus fractions in sediment and the potential mobility of phosphorus in Dianchi Lake

被引:22
作者
Li, Lingping [1 ,2 ,3 ,4 ]
Liu, Lei [3 ]
Wang, Shengrui [1 ,2 ,4 ]
Liu, Wenbin [1 ,2 ,4 ]
Jiao, Lixin [1 ,2 ,4 ]
Yang, Yang [5 ]
Yang, Rui [5 ]
机构
[1] Chinese Res Inst Environm Sci, State Key Lab Environm Criteria & Risk Assessment, Beijing 100012, Peoples R China
[2] Chinese Res Inst Environm Sci, Res Ctr Lake Ecoenvironm, State Environm Protect Key Lab Lake Pollut Contro, Beijing 100012, Peoples R China
[3] Nanchang Univ, Coll Environm & Chem Engn, Nanchang 330031, Peoples R China
[4] Yunnan Key Lab Pollut Proc & Management Plateau L, Kunming 650034, Yunnan Province, Peoples R China
[5] Yunnan Nationalities Univ, Sch Chem & Biotechnol, Kunming 650031, Peoples R China
基金
中国国家自然科学基金;
关键词
Sediment; Phosphorus fractions; Potentially mobile ability; Retention rate; LARGE SHALLOW LAKE; BOTTOM SEDIMENTS; RELEASE; WATER; CHINA; FLUXES; EUTROPHICATION; RESERVOIRS; MUGGELSEE; PROFILES;
D O I
10.1007/s12665-015-4151-y
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
In order to understand phosphorus (P) cycling and mobility in the sediment of Dianchi Lake, the spatial distribution of P fractions in surface sediment has been investigated through sequential extraction. The relationship of P fractions with the P concentrations in the overlying water, mobile P contents, and organic matters was also analyzed to determine the potential mobility and the retention effect of P in surface sediments from Dianchi Lake. Results showed that (1) the average total amount of P in the surface sediments of Dianchi Lake was 2,050.31 +/- A 620.27 mg kg(-1). The pollution levels in Caohai and in the south of Waihai were significantly higher than those in other parts of the lake. The P fractions were ranked as follows: HCl-P > NaOH-RP > Res-P > BD-P > NaOH-NRP > NH4Cl-P. Among these P fractions, NaOH-RP content (1,285.23 +/- A 1,110.51 mg kg(-1)) was highest in Caohai sediments, whereas HCl-P (925.64 +/- A 513.58 mg kg(-1)) was dominant in Waihai. (2) The average content of mobile P was 242.31 +/- A 98.11 mg kg(-1) in sediments; this value accounted for 13.54 % of total extractable P. Nonetheless, this content decreased from north to south in the lake. The average immobile P content was 1,547.22 +/- A 593.05 mg kg(-1). This value constituted 86.46 % of total extractable P. The trend of immobile P content was the opposite to that of mobile P content. (3) The P content and retention rate (66.93 %) of sediments were generally high. However, this rate was significantly lower in Caohai (13.80 %) than in Waihai (72.61 %). This result indicates that the risk of releasing the P in Caohai sediments is considerably higher than that in Waihai sediments.
引用
收藏
页码:3721 / 3731
页数:11
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