Spatial variations and distributions of phosphorus and nitrogen in bottom sediments from a typical north-temperate lake, China

被引:1
作者
Dekun Hou
Jiang He
Changwei Lü
Shengwang Dong
Jinghua Wang
Zhilei Xie
Fujin Zhang
机构
[1] University of Inner Mongolia,College of Life Science
[2] University of Inner Mongolia,Institute of Environmental Geology
[3] University of Inner Mongolia at Hohhot,College of Environment and Resources, Institute of Environmental Geology
[4] Inner Mongolia Academy of Agricultural and Animal Husbandry Sciences,Institute of Environmental Resources and Analytical Technique
来源
Environmental Earth Sciences | 2014年 / 71卷
关键词
Phosphorus; Nitrogen; Forms; Distribution characteristics; Lake Dalinouer;
D O I
暂无
中图分类号
学科分类号
摘要
Concentrations and vertical distributions of total nitrogen (TN), total phosphorus (TP) and their different forms in sediments obtained from nine locations of Lake Dalinouer in September 2008 were analyzed. The results demonstrated that TP in surface sediments ranged from 0.493 to 0.904 g/kg, and inorganic phosphorus was the main fraction of total phosphorus, ranging from 335 to 738 mg/kg. Simultaneously, the autogenetic calcium phosphorus (ACa-P) was the main fraction of inorganic phosphorus, ranging from 145.4 to 543.2 mg/kg. Vertical distribution of different phosphorus forms in different sediment cores was distinguishing, and most of them tended to increase toward the surface sediment, indicated that the phosphorus concentration was related to the humanity with a certain extent. The relationships between TP and occluded phosphorus and ACa-P were significant. Nitrogen in the sediment was composed mainly of organic nitrogen, accounting for grater than 80 % of TN. NO3−-N was the dominate fraction of inorganic nitrogen in the surface sediment, ranging between 51 and 346 mg/kg (151.1 ± 104.4 mg/kg), and accounting for between 2.2 and 17.7 % of total sediment nitrogen (6.2 ± 5.6 %). The ratio of organic carbon and TN in sediment was in range of 6.0–25.8 and presented a tendency of lake centre >lake sides, indicating that nitrogen accumulated in the sediments from lake sides came mainly from terrestrial source and nitrogen was mainly autogenetic in lake centre. Ratio of N:P in all sampling sites was below 14, indicated that N was the limiting nutrient for algal growth in this lake.
引用
收藏
页码:3063 / 3079
页数:16
相关论文
共 222 条
[41]  
Gomez E(1999)Phosphorus fractionation in volcanic lake sediments (Azores-Portugal) J Environ Monit 1 403-407
[42]  
Durillon C(2001)An investigation of the origin and mobility of phosphorus in freshwater sediments from Bort-Les-Orgues reservoir, France Fresenius J Anal Chem 370 224-228
[43]  
Rofes G(1992)Harmonized protocol and certified reference material for the determination of extractable contents of phosphorus in freshwater sediments-a synthesis of recent works Limnol Oceanogr 37 1460-1482
[44]  
Picot B(2000)Development of a sequential extraction method for different forms of phosphorus in marine sediments Water Res 34 2037-2042
[45]  
Hosomi M(2002)Potentially mobile phosphorus in Lake Erken sediment Acta Oceanol Sinica 21 125-133
[46]  
Okada M(2001)Nitrogen forms and decomposition of organic carbon in the Southern Bohai Sea core sediments Limnol Oceanogr 46 356-367
[47]  
Sudo R(2005)Effects of N:P ratio and total nutrient concentration on stream Periphyton community structure, biomass, and elemental composition Mar Geol 224 103-122
[48]  
Hu J(2001)Sea bottom in the Archipelago Sea, northern Baltic Sea-implication for phosphorus remineralization at the sediment surface Palaeogeogr Palaeo Climatol Palaeoecol 170 115-132
[49]  
Liu YD(2004)Terminal Pleistocene/Holocene palaeo-environmental changes revealed by mineral-magnetism measurements of lakes sediments for Dali Nor area, southeastern Inner Mongolia Plateau, China Palaeogeogr Palaeo Climatol Palaeoecol 208 175-193
[50]  
Liu JT(2006)Mineral magnetism of lacustrine sediments and Holocene palaeoenvironmental changes in Dali Nor area, southeast Inner Mongolia Plateau, China Eng Aspects 273 109-116