长江科学院院报 ›› 2022, Vol. 39 ›› Issue (10): 45-53.DOI: 10.11988/ckyyb.20210659

• 水环境与水生态 • 上一篇    下一篇

升钟湖夏季水和沉积物中磷形态分布特征

宋琳1,2,3, 陈超4, 冯晓玉1,2,3, 杨钻云1, 张拓1, 徐飞1, 张富斌1,2,3   

  1. 1.西华师范大学 环境科学与工程学院,四川 南充 637009;
    2.西华师范大学 国家淡水渔业工程技术研究中心(武汉)西南分中心,四川 南充 637009;
    3.西华师范大学 西南野生动植物资源保护教育部重点实验室,四川 南充 637009;
    4.四川农业大学 环境学院,成都 611130
  • 收稿日期:2021-06-28 修回日期:2021-08-31 发布日期:2022-10-13
  • 通讯作者: 张富斌(1990-),男,四川眉山人,副教授,博士,研究方向为水域生态学。E-mail: sczhangfubin@163.com
  • 作者简介:宋 琳(1997-),女,四川乐山人,硕士研究生,研究方向为水域生态学。E-mail:1576938910@qq.com
  • 基金资助:
    国家自然科学基金项目(41807458);成都市水生态文明建设研究重点项目(SST2019-2020-06)

Distribution Characteristics of Phosphorus Forms in Water and Sediment of Shengzhong Lake in Summer

SONG Lin1,2,3, CHEN Chao4, FENG Xiao-yu1,2,3, YANG Zuan-yun1, ZHANG Tuo1, XU Fei1, ZHANG Fu-bin1,2,3   

  1. 1. College of Environmental Science and Engineering,China West Normal University,Nanchong 637009,China;
    2. Southwest Branch of the National Freshwater Fishery Engineering Technology Research Center (Wuhan),China West Normal University,Nanchong 637009,China;
    3. Key Laboratory of Southwest China Wildlife Resources Conservation (Ministry of Education),China West Normal University,Nanchong 637009,China;
    4. College of Environment,Sichuan Agricultural University,Chengdu 611130,China
  • Received:2021-06-28 Revised:2021-08-31 Online:2022-10-13

摘要: 为探究升钟湖水和沉积物中磷污染情况,于2019年8月(夏季),采集了升钟湖湖区15个样点的水样和沉积物样品,测定了升钟湖表层水、间隙水及沉积物的磷形态,并分析各种形态磷之间的相关性。结果表明:①升钟湖表层水总磷含量介于0.033~0.085 mg/L,各形态的磷含量由高到低依次为DTP(61.93%)、DOP(40.00%)、PP(38.07%)和DIP(21.93%);②间隙水的总磷含量介于3.49~7.57 mg/L,是水体磷的“源”,正磷酸盐仅占总磷的1.9%;③沉积物总磷含量介于299.04~1 138.69 mg/kg,Psenner法连续分级提取出表层沉积物共有5种形态的磷,各形态磷含量由高到低依次为残渣磷(Res-P:44.78%)、金属氧化物结合态磷+有机碎屑腐殖酸磷(NaOH-P:22.92%)、钙结合态磷(HCl-P:14.82%)、可还原态磷(BD-P:13.39%)和弱吸附态磷(NH4Cl-P:4.09%),各形态磷含量均表现一定的空间分布差异,其中,总磷含量整体为西北部高于东南部;④相关性分析结果显示,沉积物中磷的释放主要通过BD-P、NaOH-P及NH4Cl-P进行,间隙水正磷酸盐(PO3-4-P)与水体各形态的磷之间均无显著的相关性(P>0.05),升钟湖沉积物磷在夏季时释放潜力较低。研究成果对于管理升钟湖的政策实施及其资源的可持续利用可提供参考。

关键词: 水和沉积物, 磷形态, 连续分级提取法, 相关性分析, 升钟湖

Abstract: The aim of this research is to investigate the phosphorus pollution in the water and sediment of the Shengzhong Lake. We collected water and sediment samples from fifteen sampling sites in the summer (August) of 2019,measured the forms of phosphorus in surface water,interstitial water and sediment,and further analyzed the correlation among various forms of phosphorus. Results revealed that the total phosphorus content in the surface water of Shengzhong Lake ranged from 0.033 mg/L to 0.085 mg/L,and the content of phosphorus in different forms were DTP (61.93%),DOP (40.00%),PP (38.07%),and DIP (21.93%),respectively. The total phosphorus content of interstitial water ranged from 3.49 mg/L to 7.57 mg/L,which is the source of phosphorus in water;however,the orthophosphate accounted for only 1.9%. Total phosphorus content of sediment ranged from 299.04 mg/kg to 1138.69 mg/kg. Five forms of phosphorus in surface sediments were extracted by continuous classification of Psenner,of which Res-P accounted for 44.78% of the total phosphorus content of the surface sediment,followed by NaOH-P occupying 22.92%,and then HCl-P 14.82%,BD-P 13.39%,and NH4Cl-P 4.09% in sequence. The content of different forms of phosphorus varied in spatial scale. Generally,the total phosphorus content in the northwest of Shengzhong Lake was higher than that in the southeast. The results of correlation analysis showed that the release of phosphorus in sediments was mainly through BD-P,NaOH-P and NH4Cl-P. No significant correlation was found between orthophosphate in interstitial water and various forms of phosphorus in water body (P > 0.05),and the release potential of phosphorus in sediments was not large in summer.

Key words: water and sediment, phosphorus form, sequential extraction method, correlation analysis, Shengzhong Lake

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