Dynamic changes of nitrogen and dissolved organic matter during the transport of mine water in a coal mine underground reservoir: Column experiments

2019 ◽  
Vol 223 ◽  
pp. 103473 ◽  
Author(s):  
Li Zhao ◽  
Chao Sun ◽  
Peixin Yan ◽  
Qing Zhang ◽  
Shidong Wang ◽  
...  
2021 ◽  
Author(s):  
Binbin Jiang ◽  
Ju Gao ◽  
Kun Du ◽  
Xu Deng ◽  
Kai Zhang

Abstract The process of water rock interaction and the purification mechanism of mine water quality were not clear after being stored in underground reservoir. This study based on the analysis of the hydrochemical characteristics of the reservoir water samples and the characterization of the rock samples, combined with PHREEQC analysis, the mechanism of water quality purification of mine water was discussed. The results showed that the rocks in the underground reservoir had layered silicate structure and flaky kaolinite structure, with some irregular edges and micro cracks, and higher specific surface area and total pore volume. These characteristics made the rocks had a certain adsorption and removal capacity for heavy metal ions and other pollutants in the mine water. The water rock interaction, such as the dissolution of albite and halite, the precipitation of gypsum and kaolinite, and the cation exchange, resulted in the increase of the concentration of Na+ and the decrease of the concentration of Ca2+, Mg2+ and TDS in the outlet water. This study also showed that PHREEQC analysis can be used to analyze the water rock interaction of coal mine underground reservoir and obtained more detailed information.


2018 ◽  
Vol 487 ◽  
pp. 76-85 ◽  
Author(s):  
Li Zhao ◽  
Yu Zhao ◽  
Xinyi Wang ◽  
Jian Yang ◽  
Shaohe Luo ◽  
...  

2012 ◽  
Vol 581-582 ◽  
pp. 1197-1201
Author(s):  
Xiao Fei Jing ◽  
Yu Long Chen ◽  
Hong Chen ◽  
Zhi Yong Cai

Biogenic gas is an important end-product of methanogenesis in an anoxic environment. Based on the coal, coal-gangue, mine water of Songzao Coal Mine and in the case of adding inoculums, the quantities of gas and the contents of methane are measured by the microorganism action, and also respectively measured fermentation broth and residues by NO3--N, NH4+-N, S2- , SO42-, the values of pH, metals and the organic matter. The results show that coal and coal-gangue are involved in the microbial role; the quantity of inoculums is directly related to the quantities of gas and the contents of methane, at the same time it has a certain degree of impact on the contents of NO3--N, NH4+ -N, S2- , SO42- and metals; besides, because of the microbial anaerobic fermentation, the contents of NH3+ are seriously substandard; overall, the group B which has a smaller proportion of coal-gangue has a less impact to the environment compared to the group A which has a larger proportion of coal-gangue. In the further research into the direction of organic matter and obtaining and using the biogas, we must prevent secondary pollution of groundwater at the same time.


2021 ◽  
Vol 7 (25) ◽  
pp. eabf4680
Author(s):  
Constanze Kuhlisch ◽  
Guy Schleyer ◽  
Nir Shahaf ◽  
Flora Vincent ◽  
Daniella Schatz ◽  
...  

Algal blooms are hotspots of primary production in the ocean, forming the basis of the marine food web and fueling the dissolved organic matter (DOM) pool. Viruses are key players in controlling algal demise, thereby diverting biomass from higher trophic levels to the DOM pool, a process termed the “viral shunt.” To decode the metabolic footprint of the viral shunt in the environment, we induced a bloom of Emiliania huxleyi and followed its succession using untargeted exometabolomics. We show that bloom succession induces dynamic changes in the exometabolic landscape. We found a set of chlorine-iodine–containing metabolites that were induced by viral infection and released during bloom demise. These metabolites were further detected in virus-infected oceanic E. huxleyi blooms. Therefore, we propose that halogenation with both chlorine and iodine is a distinct hallmark of the virus-induced DOM of E. huxleyi, providing insights into the metabolic consequences of the viral shunt.


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