Zhang Xue-qing, Xia Xing-hui, Yang Zhi-feng
State Key Joint Laboratory of Environmental Simulation and Pollution Control, School of Environment, Beijing Normal University, Beijing 100875, China.
Huan Jing Ke Xue. 2007 Sep;28(9):1954-9.
Microcosm experiments have been carried out to study the effects of suspended sediment on the transformation of organic nitrogen contaminants under different conditions, including with and without spiking bacteria to the water-sediment system. When with the natural water and sediment as cultivation media and without spiking bacteria to the water system, the presence of sediment could stimulate the transformation of organic nitrogen, and the transformation rates were correlated well with the sediment concentration. When the initial concentration of organic nitrogen in the water system was 5 mg/L, and the suspended sediment content were 0, 5 and 10 g/L, the first-order transformation rate constants of organic nitrogen were 0.286,0.333 and 0.538 d(-1), respectively; the nitrification rate constants (K4) were 0.001 8, 0.003 8 and 0.0050 L x (d x micromol)(-1), respectively, when fitting the nitrification process with the Logistic kinetics. When spiking the water systems with the same initial bacteria density, the first-order transformation rate constants of organic nitrogen and nitrification rate constants (K4) increased with the sediment content. With the natural water and sediment as cultivation media, the mechanism regarding the effects of suspended sediment on organic nitrogen transformation includes the following aspects: (1) The initial amount of bacteria increased with the sediment content in the water system. (2) The growth of bacteria was promoted by the sediments, and bacteria tended to attach to the sediment. In addition, most of organic nitrogen was attached to the sediment phase and the transformation of organic nitrogen in the water system mainly occurred at the sediment/water interface. (3) The presence of sediment increased the contact chances between bacteria and organic nitrogen, thus stimulated the transformation of organic nitrogen contaminants.
开展了微观世界实验,以研究不同条件下悬浮泥沙对有机氮污染物转化的影响,包括在水 - 泥沙系统中添加和不添加细菌的情况。以天然水和泥沙作为培养介质且未向水系统中添加细菌时,泥沙的存在能够促进有机氮的转化,且转化率与泥沙浓度具有良好的相关性。当水系统中有机氮的初始浓度为5mg/L,悬浮泥沙含量分别为0、5和10g/L时,有机氮的一级转化速率常数分别为0.286、0.333和0.538d⁻¹;采用逻辑斯蒂动力学拟合硝化过程时,硝化速率常数(K4)分别为0.0018、0.0038和0.0050L×(d×μmol)⁻¹。当向水系统中添加相同初始细菌密度时,有机氮的一级转化速率常数和硝化速率常数(K4)随泥沙含量增加而增大。以天然水和泥沙作为培养介质时,悬浮泥沙对有机氮转化影响的机制包括以下几个方面:(1)水系统中细菌的初始数量随泥沙含量增加而增多。(2)泥沙促进了细菌的生长,细菌倾向于附着在泥沙上。此外,大部分有机氮附着在泥沙相中,水系统中有机氮的转化主要发生在泥沙/水界面处。(3)泥沙的存在增加了细菌与有机氮的接触机会,从而促进了有机氮污染物的转化。