生态与农村环境学报 ›› 2022, Vol. 38 ›› Issue (8): 1076-1083.doi: 10.19741/j.issn.1673-4831.2021.0460

• 污染控制与修复 • 上一篇    下一篇

水流扰动强度对高原山地农村沟渠底泥氮释放的影响

郑淑君1, 王铁运1, 刘云根1,2, 杜鹏睿1, 王妍1,2, 贾玉洁1, 文明发3   

  1. 1. 西南林业大学生态与环境学院, 云南 昆明 650224;
    2. 云南省山地农村生态环境演变与污染治理重点实验室, 云南 昆明 650224;
    3. 云南省德源绿创环保科技有限公司, 云南 昆明 650041
  • 收稿日期:2021-07-24 出版日期:2022-08-25 发布日期:2022-08-23
  • 通讯作者: 刘云根,E-mail:henryliu1008@163.com E-mail:henryliu1008@163.com
  • 作者简介:郑淑君(1997-),女,贵州遵义人,主要研究方向为农村污水治理。E-mail:451493080@qq.com
  • 基金资助:
    国家自然科学基金(41761098,31760245)

Effect of Flow Disturbance Intensity on Nitrogen Release from Bottom Muddy of Plateau Rural Ditches

ZHENG Shu-jun1, WANG Tie-yun1, LIU Yun-gen1,2, DU Peng-rui1, WANG Yan1,2, JIA Yu-jie1, WEN Ming-fa3   

  1. 1. College of Ecology and Environment, Southwest Forestry University, Kunming 650224, China;
    2. Yunnan Key Laboratory of Ecological Environment Evolution and Pollution Control in Mountainous Rural Areas, Kunming 650224, China;
    3. Yunnan Deyuan Lüchuang Environmental Protection Technology Co. Ltd., Kunming 650041, China
  • Received:2021-07-24 Online:2022-08-25 Published:2022-08-23

摘要: 为揭示水动力扰动对高原山地农村沟渠内源氮营养盐释放的影响,通过室内模拟试验研究不同水流扰动强度(0、5、15、30、60 L·h-1)对底泥氮释放的影响。结果表明:(1)水动力扰动初期可引起底泥氮元素向上覆水释放,5 L·h-1扰动下水体中NH4+-N浓度达到最高值,60 L·h-1扰动下水体TN浓度达到最高值,在连续扰动30 d后,静置水体氮浓度高于扰动水体;(2)随扰动强度的增加,底泥TN含量也增加,但总体低于背景值,呈现出0<5<30<15<60 L·h-1的规律;(3)底泥各形态可转化态氮(TTN)含量由大到小依次表现为强氧化剂可提取态氮(SOEF-N)、强碱可提取态氮(WAEF-N)、离子交换态氮(IEF-N)和弱酸可提取态氮(SAEF-N);释放程度从易到难依次为IEF-N、WAEF-N、SAEF-N、SOEF-N;各形态氮的最小值均出现在静置时,说明扰动更有利于底泥对水体氮营养盐的吸收,减轻其沿途对周围环境造成潜在的危害。

关键词: 农村沟渠, 底泥, 氮释放, 扰动

Abstract: To investigate the effect of hydrodynamic disturbance on endogenous nitrogen (N) release in plateau mountainous rural ditches, N concentrations in overlying water under various flow disturbance intensities (0, 5, 15, 30, 60 L·h-1) were analyzed by a simulation experiment. The results show that:(1) Sediment N can be released into overlying water by the initial hydrodynamic disturbance and reaches the highest values of NH4+-N and TN at 5 and 60 L·h-1 flow disturbance intensity, respectively. After 30 days, N concentration in the undisturbed water was higher than that in the disturbed water; (2) Sediment TN contents increased with the increasing of disturbance intensity, which however were lower than the background values, showing 0 < 5 < 30 < 15 < 60 L·h-1; (3) The contents of different forms of transformable nitrogen (TTN) were in the order of strong oxidant extractable-N (SOEF-N) > strong alkali extractable-N (WAEF-N) > ion exchange-N (IEF-N) > weak acid extractable-N (SAEF-N), with releasing tendentiousness of IEF-N > WAEF-N > SAEF-N > SOEF-N. All N fractions of the sediment were at the lowest values under undisturbed treatment, indicating that the disturbance of flow benefits the N settlement in sediments, thus decreasing the risk of N to the surrounding environment.

Key words: rural ditch, sediment, nitrogen release, disturbance

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