A high-resolution dialysis technique for rapid determination of dissolved reactive phosphate and ferrous iron in pore water of sediments

被引:155
作者
Xu, Di [1 ]
Wu, Wei [2 ]
Ding, Shiming [1 ]
Sun, Qin [2 ]
Zhang, Chaosheng [3 ,4 ]
机构
[1] Chinese Acad Sci, State Key Lab Lake Sci & Environm, Nanjing Inst Geog & Limnol, Nanjing 210008, Peoples R China
[2] Hohai Univ, Coll Environm Sci & Engn, Nanjing, Jiangsu, Peoples R China
[3] Natl Univ Ireland, GIS Ctr, Ryan Inst, Galway, Ireland
[4] Natl Univ Ireland, Sch Geog & Archaeol, Galway, Ireland
关键词
Dialysis; Pore water; Peeper; Dissolved reactive phosphate; Ferrous iron; Sampling; CONSTRAINED DET; LAKE-SEDIMENTS; NATURAL-WATERS; PHOSPHORUS; SAMPLER; RELEASE; SULFATE; POREWATERS; PROFILES; SULFIDE;
D O I
10.1016/j.scitotenv.2012.01.062
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Characterization of pore water chemistry necessitates measurements of the chemical components at a high spatial resolution due to the heterogeneous nature of sediments. In this study, a novel high-resolution dialysis technique was developed for rapid sampling of dissolved reactive phosphate (DRP) and ferrous iron (Fe) in pore water at a vertical resolution of 2 mm. This technique employed a mini dialysis device (peeper) with a deployment time of 2 days in sediments for equilibration. Operational procedures following retrieval of the peeper include in situ freezing of the pore water samples through spraying commercial carbon dioxide snow, frozen storage of the pore water samples, and quick analysis of chemicals in pore water samples using 384-well microplate photometric methods. The sample consumption for each parameter can be minimized to 6 mu L, which allowed simultaneous determination of DRP and ferrous iron in a peeper device. Laboratory tests showed that the technique was robust enough for the in situ measurements. Field deployment was subsequently performed in three sites of a shallow, eutrophic bay in Lake Taihu of China. Simultaneous determination of DRP and ferrous Fe in all the sites demonstrated a similar behavior of both chemicals in the pore water profiles, verifying the control of P mobilization by Fe in sediments. (C) 2012 Elsevier B.V. All rights reserved.
引用
收藏
页码:245 / 252
页数:8
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