Effects Of Short-Term Aerobic Conditions On Phosphorus Mobility In Sediments

被引:5
|
作者
Yan, Wenming [1 ]
Liu, Ling [1 ]
Wu, Tingfeng [2 ]
Song, Lanlan [1 ]
Wang, Han [1 ,2 ]
Lu, Zhanjin [3 ]
Li, Botao [1 ]
Zhu, Yan [1 ]
机构
[1] Hohai Univ, State Key Lab Hydrol Water Resources & Hydraul En, Nanjing 210098, Jiangsu, Peoples R China
[2] Chinese Acad Sci, Nanjing Inst Geog & Limnol, State Key Lab Lake Sci & Environm, Nanjing 210008, Jiangsu, Peoples R China
[3] Chongqing Res Inst Coal Sci & Ind Grp Co Ltd, Chongqing 400039, Peoples R China
基金
国家重点研发计划; 中国国家自然科学基金;
关键词
Aerobic; Sediments; Phosphorus; Iron; Diffusive gradients in thin films; DISSOLVED REACTIVE PHOSPHORUS; THIN-FILMS TECHNIQUE; IN-SITU; DIFFUSIVE GRADIENTS; LABILE PHOSPHORUS; ALGAL BLOOMS; WATER; LAKE; IRON; RELEASE;
D O I
10.1080/02705060.2019.1659190
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
In this study, the effects of short-term aerobic conditions on phosphorus (P) mobility in sediment were investigated in the eutrophic lakes. To accomplish this, an indoor cultivation system was established and short-term cultivation (3, 8 and 15 days) was conducted under control and aerobic treatments. High-resolution diffusive gradients in thin films (DGT) and dialysis (HR-Peeper) techniques were used to determine the mobility patterns of P in sediments. The results showed that: (1) Aerobic treatment significantly increased oxygen concentrations (maximum 17.1%) in overlying water within 15 days, with no significant effects on sediment oxygen penetration depth or redox potential. Additionally, aerobic treatment inhibited soluble reactive phosphorus (SRP) and DGT-labile P release from sediment to overlying water. (2) Aerobic treatment decreased the pore water SRP and soluble Fe(II) on day 3 with no impact on sediment SRP/DGT-labile P and soluble/DGT-labile Fe on day 8 and 15. (3) Model simulation using DGT Induced Fluxes in Sediments (DIFS) showed that the pore water SRP replenishment ability of sediment particle P was lower in the aerobic group than the control group, and the sediment system equilibration time was elongated after pore water SRP decreased in the aerobic group on day 3. (4) On day 3, SRP and soluble Fe(II), DGT-labile P and DGT-labile Fe showed significant positive correlations (r > 0.888, p < 0.001), indicating that reduced pore water SRP concentration was related to decreased pore water soluble Fe(II).
引用
收藏
页码:649 / 661
页数:13
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