High-resolution imaging of labile phosphorus and its relationship with iron redox state in lake sediments
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High-resolution imaging of labile phosphorus and its relationship with iron redox state in lake sediments. / Gao, Yulu; Liang, Tao; Tian, Shuhan; Wang, Lingqing; Holm, Peter Engelund; Hansen, Hans Chr. Bruun.
I: Environmental Pollution, Bind 219, 2016, s. 466-474.Publikation: Bidrag til tidsskrift › Tidsskriftartikel › Forskning › fagfællebedømt
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T1 - High-resolution imaging of labile phosphorus and its relationship with iron redox state in lake sediments
AU - Gao, Yulu
AU - Liang, Tao
AU - Tian, Shuhan
AU - Wang, Lingqing
AU - Holm, Peter Engelund
AU - Hansen, Hans Chr. Bruun
N1 - Copyright © 2016 Elsevier Ltd. All rights reserved.
PY - 2016
Y1 - 2016
N2 - A thorough understanding of the labile status and dynamics of phosphorus (P) and iron (Fe) across the sediment-water interface (SWI) is essential for managing internal P release in eutrophic lakes. Fe-coupled inactivation of P in sediments is an important factor which affects internal P release in freshwater lakes. In this study, two in-situ high-resolution diffusive gradients in thin films (DGT) techniques, Zr-Oxide DGT and ZrO-Chelex DGT, were used to investigate the release characteristics of P from sediments in a large freshwater lake (Dongting Lake, China; area of 2691 km(2)) experiencing a regional summer algal bloom. Two-dimensional distributions of labile P in sediments were imaged with the Zr-Oxide DGT without destruction of the original structure of the sediment layer at four sites of the lake. The concentration of DGT-labile P in the sediments, ranging from 0.007 to 0.206 mg L(-1), was highly heterogeneous across the profiles. The values of apparent diffusion flux (Fd) and release flux (Fr) of P varied between -0.027-0.197 mg m(-2) d(-1) and 0.037-0.332 mg m(-2) d(-1), respectively. Labile P showed a high and positive correlation (p < 0.01) with labile Fe(II) in the profiles, providing high-resolution evidence for the key role of Fe-redox cycling in labile P variation in sediments.
AB - A thorough understanding of the labile status and dynamics of phosphorus (P) and iron (Fe) across the sediment-water interface (SWI) is essential for managing internal P release in eutrophic lakes. Fe-coupled inactivation of P in sediments is an important factor which affects internal P release in freshwater lakes. In this study, two in-situ high-resolution diffusive gradients in thin films (DGT) techniques, Zr-Oxide DGT and ZrO-Chelex DGT, were used to investigate the release characteristics of P from sediments in a large freshwater lake (Dongting Lake, China; area of 2691 km(2)) experiencing a regional summer algal bloom. Two-dimensional distributions of labile P in sediments were imaged with the Zr-Oxide DGT without destruction of the original structure of the sediment layer at four sites of the lake. The concentration of DGT-labile P in the sediments, ranging from 0.007 to 0.206 mg L(-1), was highly heterogeneous across the profiles. The values of apparent diffusion flux (Fd) and release flux (Fr) of P varied between -0.027-0.197 mg m(-2) d(-1) and 0.037-0.332 mg m(-2) d(-1), respectively. Labile P showed a high and positive correlation (p < 0.01) with labile Fe(II) in the profiles, providing high-resolution evidence for the key role of Fe-redox cycling in labile P variation in sediments.
U2 - 10.1016/j.envpol.2016.05.053
DO - 10.1016/j.envpol.2016.05.053
M3 - Journal article
C2 - 27376987
VL - 219
SP - 466
EP - 474
JO - Environmental Pollution
JF - Environmental Pollution
SN - 0269-7491
ER -
ID: 169107145