内蒙古农业大学 水利与土木建筑工程学院,内蒙古,呼和浩特,010018
纸质出版:2018
移动端阅览
杨旭, 李畅游, 李文宝, 等. 达里诺尔湖磷赋存特征及底泥释放影响因素[J]. 水土保持通报, 2018,38(4):92-97.
YANG Xu, LI Changyou, LI Wenbao, et al. Characteristics of Phosphorus Occurrence and Influence Factors of Sediment Release in Dali-Nor Lake[J]. Bulletin of Soiland Water Conservation, 2018, 38(4): 92-97.
杨旭, 李畅游, 李文宝, 等. 达里诺尔湖磷赋存特征及底泥释放影响因素[J]. 水土保持通报, 2018,38(4):92-97. DOI: 10.13961/j.cnki.stbctb.2018.04.015.
YANG Xu, LI Changyou, LI Wenbao, et al. Characteristics of Phosphorus Occurrence and Influence Factors of Sediment Release in Dali-Nor Lake[J]. Bulletin of Soiland Water Conservation, 2018, 38(4): 92-97. DOI: 10.13961/j.cnki.stbctb.2018.04.015.
[目的]揭示封闭性内陆湖磷组成特点及底泥释放影响因素,为控制达里湖磷元素污染提供理论支持。[方法]对达里诺尔湖水体总磷(TP)、溶解性总磷(DTP)、溶解性无机磷(DIP),沉积物形态磷进行监测,并利用因子分析的方法对影响沉积物底泥释放的因素分类讨论。[结果]达里湖上覆水总磷(TP)均值2.00±0.02 mg/L,间隙水TP均值2.50±0.02 mg/L,沉积物TP在206.09~940.49 mg/kg之间。沉积物中无机磷(IP)占TP的47.9%,是沉积物主要的磷形态之一。钙磷(Ca-P)是IP中含量最多的形态磷(217.76±47.01 mg/kg),其次为铁铝结合态磷(Fe/Al-P,62.73±28.34 mg/kg)和交换态磷(Ex-P,36.50±19.13 mg/kg),有机磷(OP,200.28±135.13 mg/kg)含量占TP的41.8%;通过因子分析法将影响底泥释放的因素分为三类:沉积物TP,Ca-P,Fe/Al-P和生物有效性磷含量归为沉积物磷因子;水体pH,DO,Eh值以及间隙水磷含量归为界面影响因子;湖水水深归为湖泊自身特征因子。[结论]达里湖存在沉积物磷底泥释放的风险,根据因子分析的结果可知,影响沉积物底泥释放的因素分为沉积物磷、水—沉积物界面理化指标和湖水水深3大类。
[Objective] In order to reveal the characteristics of phosphorus composition in closed inland lake
and the influencing factors of endogenous release.[Methods] The phosphorus content in different medium of Dali-Nor Lake was determined. Using factor analysis to classify the factors affecting sediment release.[Results] The average value of total phosphorus (TP) in the water on Dali-Nor Lake was 2.00±0.02 mg/L
and the mean value of interstitial water TP was 2.50±0.02 mg/L. The sediment TP is between 206.09 to 940.49 mg/kg. Inorganic phosphorus (IP) in sediments accounts for 47.9% of TP
which is one of the main forms of phosphorus in sediments. Followed by iron-aluminum bound phosphorus (Fe/Al-P
62.73±28.34 mg/kg) and exchangeable phosphorus (Ex-P
36.50±19.13 mg/kg) By using the factor analysis method to analyze the influence of 13 sediments release indicators
there are 4 main factors
the 13 indexes are divided into 3 categories:TP
Ca-P
Fe/Al-P and bioavailability of phosphorus content in sediments classified as phosphorus in sediments and interstitial water factor; phosphorus concentrations of pH
DO
Eh of the water as the interface influence factor; The third is water depth to lakes characteristic factor.[Conclusion] There is a risk of release of sediment phosphorus sediment in Dali-Nor Lake. According to the results of factor analysis
the factors affecting sediment release are divided into three categories:sediment phosphorus
water-sediment interface physical and chemical indicators and lake water depth.
国家环境保护总局.2016年中国环境状况公报[J].环境保护,2016(7):17-25.
Spears B M, Carvalho L, Perkins R, et al. Sediment phosphorus cycling in a large shallow lake:Spatio-temporal variation in phosphorus pools and release[J].Hydrobiologia, 2007,584(1):37-48.
Komatsu E, Fukushima T, Shiraishi H. Modeling of P-dynamics and algal growth in a stratified reservoir-mechanisms of P-cycle in water and interaction between overlying water and sediment[J].Ecological Modelling, 2006,197(3):331-349.
Ruban V, López-Sánchez J F, Pardo P, et al. Harmonized protocol and certifiedreference materialfor the determination of extractablecontents of phosphorus in freshwater sediments:A synthesis of recent works[J].Fresenius Journal of Analytical Chemistry, 2001,370(2):224-228.
Boström B, Andersen J M, Fleischer S, et al. Exchange of phosphorus across the sediment-water interface[J]. Hydrobiologia, 1988,170(1):229-244.
Grandel S, Rickert D, Schlüter M, et al. Pore-water distribution and quantification of diffusive benthic fluxes of silicic acid, nitrate and phosphate in surface sediments of the deep Arabian Sea[J]. Deep Sea Research(Part Ⅱ):Topical Studies in Oceanography, 2000,47(14):2707-2734.
Sondergaard M, Phillips G, Hellsten S, et al.Maximum growing depth of submerged macrophytes in European lakes[J].Hydrobiologia, 2013,704(1):165-177.
史静,俎晓静,张乃明,等.滇池草海沉积物磷形态、空间分布特征及影响因素[J].中国环境科学,2013,33(10):1808-1813.
金晓丹,吴昊,陈志明,等.长江河口水库沉积物磷形态、吸附和释放特性[J].环境科学,2015,36(2):448-456.
李乐,王圣瑞,焦立新,等.滇池柱状沉积物磷形态垂向变化及对释放的贡献[J].环境科学, 2016, 37(9):3384-3393.
向速林,陶术平,吴代赦.鄱阳湖沉积物和水界面磷的交换通量[J].湖泊科学,2017,29(2):326-333.
李文宝,李畅游,刘晓旭,等.达里诺尔湖水体稳定氢、氧同位素组成变化对结冰过程的响应[J].中国地质大学学报:地球科学,2015,40(12):2081-2090.
赵胜男,史小红,崔英,等.内蒙古达里诺尔湖湖泊水体与入湖河水水化学特征及控制因素[J].环境化学,2016,35(9):1865-1875.
国家环保局本书编委会. 水和废水监测分析方法[M].北京:中国环境科学出版社, 1989.
Ruban V. Harmonized protocol and certified reference material for the determination of extractable contents of phosphorus in freshwater sediments:A synthesis of recent works[J]. Fresenius Journal of Analytical Chemistry, 2001,370(2/3):224-228.
Yu Qing, Wang Hongzhu, Li Yan, et al.Effects of high nitrogen concentrations on the growth of submersed macrophytes at moderate phosphorus concentrations[J].Water Research, 2015,83:385-395.
郭霞.内蒙古高原典型湖泊磷的地球化学特征[D].内蒙古呼和浩特:内蒙古大学, 2014.
郑西来,张俊杰,陈蕾.再悬浮条件C内源磷迁移-转化机制研究进展[J].水科学进展,2013, 24(2):287-295.
刘志娇.达里诺尔湖水动力条件试验及氢氧稳定同位素研究[D].内蒙古呼和浩特:内蒙古农业大学,2015.
王志齐,李宝,梁仁君,等.南四湖沉积物磷形态及其与间隙水磷的相关性分析[J].环境科学学报,2013,33(1):139-146.
温胜芳,单保庆,张洪.巢湖表层沉积物磷的空间分布差异性研究[J].环境科学,2012,33(7):2322-2329.
何江,孙英,吕昌伟,等.岱海表层沉积物中内源磷的释放[J].生态学报,2010,20(2):389-398.
Chuai Xiaoming, Ding Wei, Chen Xiaofeng, et al. Phosphorus release from cyanobacterial blooms in Meiliang Bay of Lake Taihu, China[J]. Ecological Engineering, 2011,37(6):842-849.
高春梅,朱珠,王功芹,等.海州湾海洋牧场海域表层沉积物磷形态与环境意义[J].中国环境科学,2015,235(11):3437-3444.
Liu Sumei, Zhang Jing, Li Daoji. Phosphorus cycling in sediments of the Bohaiand Yellow seas[J]. Estuarine, Coast aland Shelf Science, 2004,59(2):209-218.
张路,范成新,朱广伟,等.长江中下游湖泊沉积物生物可利用磷分布特征[J].湖泊科学,2006,18(1):36-42.
朱广伟,秦伯强.沉积物中磷形态的化学连续提取法应用研究[J].农业环境科学学报,2003,22(3):349-352.
张志斌,张学杨,张波,等.南四湖微山湖区沉积物磷形态分布特征[J].环境科学,2009,30(5):1345-1350.
0
浏览量
990
下载量
4
CSCD
关联资源
相关文章
相关作者
相关机构
京公网安备11010802024621