Evidence map›Paper›PMID 36278070›Full record

ArticleACS omega2022

Insight into the Process and Mechanism of Water-Rock Interaction in Underground Coal Mine Reservoirs Based on Indoor Static Simulation Experiments.

Kai Zhang, Xu Deng, Ju Gao, Shuyu Liu, Fuyao Wang, Jinglong Han

Open access · goldAbstract read
In one paragraph

Article in ACS omega, 2022. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 6 papers.

0numbers the graph read from it
0cells of the map it votes in
6citing papers in PubMed
2.0field-weighted citation impact, top 15% of its field
1 · What the graph read from it

What it found

Each row is one number read from the abstract, on the scale the paper reported it, with its interval. Left of the dashed line favours the treatment, right favours the comparator. Under each row is the sentence it came from. New to these charts? A ten-minute tutorial.

The abstract states no effect estimate the extractor could read, or names no intervention and outcome on the map, so this paper lights no cell and moves no belief. It is still indexed, cited and linked below.

2 · The registry

The trial behind it

Trials whose registry record cites this paper, or whose number appears in the abstract. A trial that started after this paper was published is citing it as background, not reporting it.

Neither the registry nor the abstract names a trial number. If this is a trial report, that itself is worth knowing.

3 · Its place in the literature

Who cites it

6 citing papers in PubMed, 21 citations in OpenAlex.

  1. Article
  2. Article
  3. Article
  4. Article
  5. Review
  6. Mechanism of Changes in Goaf Water Hydrogeochemistry: A Case Study of the Menkeqing Coal Mine.International journal of environmental research and public health · 2022
    Article
4 · The record

Corrections and comments

PubMed lists nothing against this paper. Absence here is not a guarantee, only a check that was made.

5 · Who and what money

Authors and funding

6 authors at 1 institution in 1 country.

Kai ZhangSchool of Chemistry and Environment, China University of Mining and Technology (Beijing), Beijing, 100083, China.ORCID https://orcid.org/0000-0001-7735-7663
Xu DengSchool of Chemistry and Environment, China University of Mining and Technology (Beijing), Beijing, 100083, China.
Ju GaoSchool of Chemistry and Environment, China University of Mining and Technology (Beijing), Beijing, 100083, China.
Shuyu LiuSchool of Chemistry and Environment, China University of Mining and Technology (Beijing), Beijing, 100083, China.
Fuyao WangSchool of Chemistry and Environment, China University of Mining and Technology (Beijing), Beijing, 100083, China.
Jinglong HanSchool of Chemistry and Environment, China University of Mining and Technology (Beijing), Beijing, 100083, China.
China University of Mining and Technology · CN

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

During the storage of underground water reservoirs in coal mines, water-rock interaction occurred between mine water and collapsed rocks, resulting in improved mine water quality, but the water-rock process and mechanism have not been clarified. In this study, six sets of simulated experiments were designed to investigate the water-rock interaction between two types of roof collapse rocks and different water samples in the Daliuta coal mine. The ion ratio method and multivariate statistics are used to reveal the process and mechanism of water-rock interaction during the experimental process from the perspective of input and output water chemical characteristics and rock properties, respectively. The results show that the ion concentration of the effluent water is controlled by water-rock interaction, and the water-rock process mainly involves the dissolution of halite, silicate, pyrite, calcite, dolomite, magnesia chlorite, and gypsum precipitation and is accompanied by ion exchange. Mineral dissolution and precipitation are the most important factors affecting the ion abundance in the effluent. There are differences in the reaction rate, degree of reaction, and dissolution process during the experimental process of fine sandstone and mudstone. Fine sandstone is more reactive than mudstone in terms of reaction rate and degree of reaction, and fine sandstone is dissolved from surface pores to inside and around, while mudstone is generated in new dissolved pores. We found that rock type, ion concentration in the input water, and rock reaction period influence the water-rock interaction during the experiment. The results provide a reference for clarifying the water-rock interaction during the storage of underground water reservoirs in coal mines and predicting the water quality of the effluent.

Identifiers

PMID36278070
PMCPMC9583642
OpenAlexW4302425119

What OpenQuestion holds

Textmetadata
LicenceCC BY-NC-ND
Read underepoch 390

Registered trials

None linked

Read under generation 80e0d062 · epoch 390. Bibliography from PubMed, PubMed Central and OpenAlex; grants from NIH RePORTER; trial links from ClinicalTrials.gov; estimates, votes and beliefs from the OpenQuestion graph.