首页 | 本学科首页   官方微博 | 高级检索  
     

源头溪流氮磷耦合吸收效应及动力学模拟
引用本文:李如忠,许大强,阙凤翔. 源头溪流氮磷耦合吸收效应及动力学模拟[J]. 中国环境科学, 2019, 39(2): 648-656
作者姓名:李如忠  许大强  阙凤翔
作者单位:合肥工业大学资源与环境工程学院, 安徽 合肥 230009
基金项目:国家自然科学基金资助项目(51579061)
摘    要:为揭示源头溪流氮磷耦合吸收作用机制,选择NaCl和NaBr为保守型示踪剂、KNO3和KH2PO4为添加营养盐,于2017年10月~2018年3月在合肥城郊的2条源头溪流,开展5次由单、双营养盐添加构成的示踪试验,利用TASCC技术方法,分别以Michaelis-Menten(M-M)方程和双营养耦合吸收曲面模型拟合营养盐吸收动力学过程.结果表明,双添加试验的NO3-N、PO4-P吸收速率均明显高于单添加情形,意味着溪流中NO3-N与PO4-P吸收存在相互促进作用;双营养耦合吸收响应曲面直观展示了氮、磷营养盐不同浓度水平及浓度比情形下吸收速率的演化趋势,诠释了较低浓度水平下溪流NO3-N(或PO4-P)吸收速率随PO4-P(或NO3-N)可利用量增加而增大的作用机制;两种动力学模型在NO3-N、PO4-P最大吸收速率拟合结果上均存在不同程度的偏差,其中M-M方程低估了Umax-N和Umax-P,相应幅度分别达3.91%~16.11%、3.23%~23.63%.

关 键 词:源头溪流  氮磷耦合吸收  TASCC  Michaelis-Menten (M-M)方程  响应曲面模型  
收稿时间:2018-07-02

Coupling uptake kinetics and mechanism of nitrogen and phosphorus in headwater streams
LI Ru-zhong,XU Da-qiang,QUE Feng-xiang. Coupling uptake kinetics and mechanism of nitrogen and phosphorus in headwater streams[J]. China Environmental Science, 2019, 39(2): 648-656
Authors:LI Ru-zhong  XU Da-qiang  QUE Feng-xiang
Affiliation:School of Resources and Environmental Engineering, Hefei University of Technology, Hefei 230009, China
Abstract:Five conservative tracer tests including single nutrient and dual-nutrient injection were conducted to reveal the coupling mechanism of nitrogen and phosphorus uptake in two headwater streams of Ershibu River in the suburb of Hefei, Chaohu Lake Basin, from October 2017 to March 2018. NaCl and NaBr were selected as the conservative tracers; the reactive nutrients were KNO3 and KH2PO4. Based on the TASCC (Tracer Additions for Spiraling Curve Characterization) method, the Michaelis-Menten (M-M) model and the two-substrate M-M response surface model were applied to simulate the kinetics of nutrients uptake. The results showed that the uptake rates of NO3-N and PO4-P in the dual-nutrient injection test were significantly higher than those obtained in the single nutrient injection test, which implied that mutual promotion between NO3-N and PO4-P for nutrient uptake in the two headwater streams. The dual-nutrient uptake response surfaces presented the evolutionary trends of uptake rates at different concentrations and ratios of nitrogen and phosphorus. Additionally, it also explained the interaction mechanism of NO3-N (or PO4-P) uptake rate increasing with the increase of the available PO4-P (or NO3-N) at their low concentration. The fitting results of NO3-N and PO4-P maximum uptake rates (Umax-N and Umax-P) obtained by the two kinetic models presented deviations in a certain degree. The parameters of Umax-N and Umax-P were underestimated by the M-M model ranging from 3.91%~16.11% and 3.23%~23.63%, respectively.
Keywords:headwater stream  coupling uptake of nitrogen and phosphorus  TASCC  Michaelis-Menten (M-M) model  response surface model  
本文献已被 CNKI 等数据库收录!
点击此处可从《中国环境科学》浏览原始摘要信息
点击此处可从《中国环境科学》下载全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号