2022
DOI: 10.1016/j.conbuildmat.2021.125862
|View full text |Cite
|
Sign up to set email alerts
|

Bioweathering of minerals and dissolution assessment by experimental simulations—Implications for sandstone rocks: A review

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
2
1

Citation Types

0
16
0

Year Published

2022
2022
2024
2024

Publication Types

Select...
6
1

Relationship

0
7

Authors

Journals

citations
Cited by 26 publications
(16 citation statements)
references
References 214 publications
0
16
0
Order By: Relevance
“…The B-H was formed in situ inside the pores of sandstones; there is excellent compatibility with the sandstone, resulting in strengthening. Strong hydrogen bonding, coordination, ionic bonding, and favorable mechanical fitting between the hydrogel and the sandstone are factors that made the sandstone more robust: (1) strong hydrogen bonds: The hydrogel contains many amino groups, which could form extremely strong hydrogen bonds with sandstone (Si–OH). , (2) The Si 4+ and interlayer Al 3+ in the Si–O of the bentonite itself were easily replaced by low-valent ions such as Mg 2+ , Fe 2+ , and Li + , causing the bentonite layer to have a net negative charge; it then could interact with metal cations in the sandstone rock matrix to generate ionic bonds. , (3) Sandstone contains metal ions that can form coordination bonds with amino groups in the hydrogel. , (4) The excellent mechanical fit between the hydrogel and the pores of sandstones is a further strengthening factor.…”
Section: Resultsmentioning
confidence: 99%
See 3 more Smart Citations
“…The B-H was formed in situ inside the pores of sandstones; there is excellent compatibility with the sandstone, resulting in strengthening. Strong hydrogen bonding, coordination, ionic bonding, and favorable mechanical fitting between the hydrogel and the sandstone are factors that made the sandstone more robust: (1) strong hydrogen bonds: The hydrogel contains many amino groups, which could form extremely strong hydrogen bonds with sandstone (Si–OH). , (2) The Si 4+ and interlayer Al 3+ in the Si–O of the bentonite itself were easily replaced by low-valent ions such as Mg 2+ , Fe 2+ , and Li + , causing the bentonite layer to have a net negative charge; it then could interact with metal cations in the sandstone rock matrix to generate ionic bonds. , (3) Sandstone contains metal ions that can form coordination bonds with amino groups in the hydrogel. , (4) The excellent mechanical fit between the hydrogel and the pores of sandstones is a further strengthening factor.…”
Section: Resultsmentioning
confidence: 99%
“…Major ancient sandstone artifacts are generally outdoors and subject to environmental factors. , In particular, acid rain can be lethal. , We evaluated the acid resistance of B-H–sandstone (Figure a). Compared with the complete degradation unprotected sandstone can undergo, the acid resistance of B-H–sandstone was greatly improved (88.83% residual mass).…”
Section: Resultsmentioning
confidence: 99%
See 2 more Smart Citations
“…Moreover, the presence of acidic solutions in rocks creates a corrosive effect, and the H + ions in the solution react with feldspar, mica, and calcite in the sandstone. These acid–rock reactions promote the creation of secondary pores and material dissolution, and, therefore, a prominent reduction in host rock strength is observed . Therefore, it is evident that the understanding of chemical diagenesis is of great importance in predicting reservoir behavior and hydrocarbon accumulation as it clearly affects the subsurface distribution of the porosity, permeability, and, thus, economic value of a specific sandstone reservoir …”
Section: Introductionmentioning
confidence: 99%