Microbiological factors of the formation of iron-containing minerals

被引：2
|
作者：
Kondratyeva, L. M. [1 ]
Golubeva, E. M. [2 ]
Litvinenko, Z. N. [3 ]
机构：
[1] Russian Acad Sci, Inst Water & Ecol Problems, Far East Branch, Ul Dikopoltseva 56, Khabarovsk 680000, Russia
[2] Russian Acad Sci, Kosygin Inst Tecton & Geophys, Far East Branch, Ul Kim Yu Chena 65, Khabarovsk 680000, Russia
[3] Khabarovsk Municipal Unitary Enterprise Vodocanal, Per Topog Sky 12, Khabarovsk 680000, Russia
来源：
CONTEMPORARY PROBLEMS OF ECOLOGY | 2016年 / 9卷 / 03期
关键词：
underground waters; organic matter; biofilm; biomineral; goethite; BIOMINERALIZATION; GOETHITE; BIOFILM;
D O I：
10.1134/S1995425516030070
中图分类号：
Q14 [生态学（生物生态学）];
学科分类号：
071012 ; 0713 ;
摘要：
In the present study, the process of biofilm formation in iron-containing aqueous medium in the presence of different organic compounds with different bioavailability (yeast extract, peptone, and humic substances) is considered. Investigations conducted using a scanning electronic microscope and X-ray diffraction analysis allow us to reveal the presence of biologically produced goethite (alpha-FeOOH) in the crystal structure. It was supposed that the supply of surface waters contaminated with organic compounds to ironcontaining underground waters could increase the risk of plugging aquifer pore space by biogenic iron-containing minerals.
引用
收藏
页码：318 / 328
页数：11
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