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In situ, high-resolution imaging of labile phosphorus in sediments of a large eutrophic lake

机译:大型富营养化湖泊沉积物中不稳定磷的高分辨率原位成像

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摘要

Understanding the labile status of phosphorus (P) in sediments is crucial for managing a eutrophic lake, but it is hindered by lacking in situ data particularly on a catchment scale. In this study, we for the first time characterized in situ labile P in sediments with the Zr-oxide diffusive gradients in thin films (Zr-oxide DGT) technique at a two-dimensional (2D), submillimeter resolution in a large eutrophic lake (Lake Taihu, China, with an area of 2338 km(2)). The concentration of DGT-labile P in the sediment profiles showed strong variation mostly ranging from 0.01 to 0.35 mg L-1 with a considerable number of hotspots. The horizontal heterogeneity index of labile P varied from 0.04 to 4.5. High values appeared at the depths of 0-30 mm, likely reflecting an active layer of labile P under the sediment -water interface (SWI). Concentration gradients of labile P were observed from the high-resolution 1D DGT profiles in both the sediment and overlying water layers close to the SWI. The apparent diffusion flux of P across the SWI was calculated between -21 and 65 ng cm(-2) d(-1), which showed that the sediments tended to be a source and sink of overlying water P in the algal- and macrophyte-dominated regions, respectively. The DGT-labile P in the 0-30 mm active layer showed a better correlation with overlying water P than the labile P measured by ex situ chemical extraction methods. It implies that in situ, high-resolution profiling of labile P with DGT is a more reliable approach and will significantly extend our ability in in situ monitoring of the labile status of P in sediments in the field. (C) 2015 Elsevier Ltd. All rights reserved.
机译:了解沉积物中磷(P)的不稳定状态对于管理富营养化湖泊至关重要,但是由于缺乏现场数据(尤其是流域规模)而受到阻碍。在这项研究中,我们首次使用二维(2D)亚毫米分辨率的大型富营养化湖泊(2D)中薄膜的Zr-氧化物扩散梯度(Zr-氧化物DGT)技术表征了沉积物中的原位不稳定P.中国太湖,面积2338公里(2))。沉积物剖面中DGT不稳定的P的浓度显示出很大的变化,大部分在0.01至0.35 mg L-1范围内,并具有大量热点。不稳定P的水平异质性指数在0.04至4.5之间变化。高值出现在0-30 mm的深度处,可能反映了沉积物-水界面(SWI)下不稳定磷的活性层。从高分辨率的1D DGT剖面中,在靠近SWI的沉积物和上覆水层中都观察到了不稳定P的浓度梯度。 P在SWI上的表观扩散通量计算为-21至65 ng cm(-2)d(-1),这表明沉积物倾向于是藻类和大型植物中上覆水P的源和汇。 -主要地区。在0-30 mm的活性层中,DGT不稳定的P与上层水P的相关性比通过异位化学提取方法测得的不稳定的P更好。这意味着用DGT对不稳定的P进行原位高分辨率剖析是一种更可靠的方法,它将大大扩展我们在现场监测沉积物中P的不稳定状态的能力。 (C)2015 Elsevier Ltd.保留所有权利。

著录项

  • 来源
    《Water Research》 |2015年第1期|100-109|共10页
  • 作者单位

    Chinese Acad Sci, Nanjing Inst Geog & Limnol, State Key Lab Lake Sci & Environm, Nanjing 210008, Jiangsu, Peoples R China;

    Chinese Acad Sci, Nanjing Inst Geog & Limnol, State Key Lab Lake Sci & Environm, Nanjing 210008, Jiangsu, Peoples R China;

    Nanjing Forestry Univ, Coll Forest Resources & Environm, Nanjing 210037, Jiangsu, Peoples R China;

    Chinese Acad Sci, Nanjing Inst Geog & Limnol, State Key Lab Lake Sci & Environm, Nanjing 210008, Jiangsu, Peoples R China;

    Chinese Acad Sci, Nanjing Inst Geog & Limnol, State Key Lab Lake Sci & Environm, Nanjing 210008, Jiangsu, Peoples R China;

    Chinese Acad Sci, Nanjing Inst Geog & Limnol, State Key Lab Lake Sci & Environm, Nanjing 210008, Jiangsu, Peoples R China;

    Hohai Univ, Coll Environm, Minist Educ, Key Lab Integrated Regulat & Resource Dev Shallow, Nanjing 210098, Jiangsu, Peoples R China;

    Queens Univ Belfast, Sch Biol Sci, Inst Global Food Secur, Belfast BT9 7BL, Antrim, North Ireland;

    Natl Univ Ireland, GIS Ctr, Ryan Inst, Galway, Ireland|Natl Univ Ireland, Sch Geog & Archaeol, Galway, Ireland;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Eutrophication; High resolution; Phosphorus; Sediment-water interface; Zr-oxide DGT;

    机译:富营养化;高分辨率;磷;沉积物-水界面;Zr-氧化物DGT;

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