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阿哈水库沉积物-水界面磷、 铁、 硫高分辨率空间分布特征
High-resolution Distribution Characteristics of Phosphorous, Iron and Sulfur Across the Sediment-Water Interface of Aha Reservoir

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孙清清 1   陈敬安 1 *   王敬富 1   杨海全 1   计永雪 1   兰晨 1   王箫 2  
文摘 选取贵州典型高原亚深水型湖库阿哈水库为研究对象,利用薄膜扩散梯度技术获取夏季分层期不同湖区沉积物-水界面磷、 铁、 硫的原位、 二维高分辨分布信息,并结合水化学及沉积物磷形态分析,探讨了沉积物P-Fe-S分布规律及控制因素. 结果表明:沉积物-水界面DGT-P的浓度变化范围0.00~0.43 mg·L~(-1),DGT-Fe的浓度变化范围0.00~2.83 mg·L~(-1),DGT-S的浓度变化范围0.00~0.10 mg·L~(-1). 阿哈水库沉积物孔隙水磷、 铁、 硫浓度在垂向分布上没有显著的相关性,DGT-P、 DGT-Fe甚至还呈反向变化,这与很多湖泊的研究结果存在明显差异,其原因可能是阿哈水库沉积物具有很高的Fe/P和Fe/S比值,过剩的Fe导致还原态S以FeS/FeS_2形式沉淀后,P仍然被Fe(Ⅲ)固定在沉积物中. 阿哈水库沉积物磷形态以NaOH-SRP和BD-P为主,NaOH-SRP含量变化范围为192~604 mg·kg~(-1),平均值约为392 mg·kg~(-1),BD-P含量变化范围为143~524 mg·kg~(-1),平均值约为225 mg·kg~(-1). 阿哈水库底层水体长期处于厌氧环境,Fe、 S地球化学循环对沉积物内源磷释放起着重要控制作用.
其他语种文摘 In situ two-dimension, high-resolution distribution of phosphorus(P), iron(Fe), sulfur(S) from the sediment-water interface was investigated in different areas of Aha Reservoir, a typical sub-deep water lake, using diffusive gradients in thin films(DGT) technique, combining with water chemistry and sedimentary phosphorus speciation analysis, aimed to discuss the distribution and control factors of P-Fe-S in sediments. DGT-P ranged from 0.00 mg·L~(-1)to 0.43 mg·L~(-1). DGT-Fe rangd from 0.00 mg·L~(-1)to 2.83 mg·L~(-1). DGT-S ranged from 0.00 mg·L~(-1)to 0.10 mg·L~(-1). There was no significant correlation among the concentrations of P, Fe, S in the sediment pore water of Aha Reservoir, which is markedly different from the results of previous studies. We hypothesize that the high ratios of Fe/P and Fe/S induced the direct reaction of surplus Fe(Ⅲ) with S~(2-), yielding FeS and/or FeS_2, while P was firmly fixed in sediments by Fe(Ⅲ). NaOH-SRP(ranging between 192 and 604 mg·kg~(-1)) and BD-P(ranging between 143 and 524 mg·kg~(-1)) were the two major fractions of P in sediments. Since the environment for the bottom layer of water in Aha Reservoir is anoxic, the geochemical cycle of Fe and S potentially has a massive impact on the activation and migration of sedimentary P.
来源 环境科学 ,2017,38(7):2810-2818 【核心库】
DOI 10.13227/j.hjkx.201611159
关键词 阿哈水库 ; 沉积物-水界面 ; 薄膜扩散梯度技术 ; ; ;
地址

1. 中国科学院地球化学研究所, 环境地球化学国家重点实验室, 贵阳, 550081  

2. 贵州师范大学地理与环境科学学院, 贵阳, 550025

语种 中文
文献类型 研究性论文
ISSN 0250-3301
学科 环境污染及其防治
基金 国家自然科学基金项目 ;  贵州省应用基础研究计划重大项目 ;  贵州省项目 ;  贵州省项目
文献收藏号 CSCD:6021260

参考文献 共 47 共3页

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引证文献 14

1 杨梦迪 梯级水库群水体碳、硫元素循环及耦合效应——以嘉陵江为例 生态学杂志,2018,37(3):651-660
CSCD被引 10

2 王敬富 底泥疏浚对阿哈水库内源污染的影响 环境工程,2018,36(3):69-73,147
CSCD被引 7

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