Gel-Based Coloration Technique for the Submillimeter-Scale Imaging of Labile Phosphorus in Sediments and Soils with Diffusive Gradients in Thin Films

被引:110
作者
Ding, Shiming [1 ]
Wang, Yan [1 ]
Xu, Di [1 ]
Zhu, Chungang [2 ]
Zhang, Chaosheng [3 ,4 ]
机构
[1] Chinese Acad Sci, Nanjing Inst Geog & Limnol, State Key Lab Lake Sci & Environm, Nanjing 210008, Jiangsu, Peoples R China
[2] Southeast Univ, Sch Civil Engn, Nanjing 210096, 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
DISSOLVED REACTIVE PHOSPHORUS; IN-SITU MEASUREMENT; HIGH-RESOLUTION; NATURAL-WATERS; DGT TECHNIQUE; PHOSPHATE; SULFIDE; LAKE; FRACTIONATION; PERFORMANCE;
D O I
10.1021/es400192j
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
We report a highly promising technique for the high-resolution imaging of labile phosphorus (P) in sediments and soils in combination with the diffusive gradients in thin films (DGT). This technique was based on the surface coloration of the Zr-oxide binding gel using the conventional molybdenum blue method following the DGT uptake of P to this gel. The accumulated mass of the P in the gel was then measured according to the grayscale intensity on the gel surface using computer. imaging densitometry. A pretreatment of the gel in hot water (85 degrees C) for 5 d was required to immobilize the phosphate and the formed blue complex in the gel during the color development. The optimal time required for a complete color development was determined to be 45 min. The appropriate volume of the coloring reagent added was 200 times of that of the gel. A calibration equation was established under the optimized conditions, based on which a quantitative measurement of P was obtained when the concentration of P in solutions ranged from 0.04 mg L-1 to 4.1 mg L-1 for a 24 h deployment of typical DGT devices at 25 degrees C. The suitability of the coloration technique was well demonstrated by the observation of small, discrete spots with elevated P concentrations in a sediment profile.
引用
收藏
页码:7821 / 7829
页数:9
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