2007
DOI: 10.1016/s1002-0160(07)60012-5
|View full text |Cite
|
Sign up to set email alerts
|

Hydrolysis of Aluminum Ions in Kaolinite and Oxisol Suspensions as Influenced by Organic Anions

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1

Citation Types

0
3
0

Year Published

2009
2009
2023
2023

Publication Types

Select...
7

Relationship

0
7

Authors

Journals

citations
Cited by 7 publications
(3 citation statements)
references
References 17 publications
0
3
0
Order By: Relevance
“…However, soils at this site also contained a relatively high concentration of extractable Al, presumably in the form of aluminum sulfate salts ( Supplemental Table S1), which may indicate the continued oxidation of sulfide ore. The formation of aluminum salts in the 3.6 to 4.5 pH range is consistent with the release of H + ions during oxidation of sulfide ores, counteracting the effect of the dolostone (Xu et al, 2007;Jones et al, 2011). Alternatively, as these soils were exposed to sulfuric acid deposition, there should have been sufficient sulfate available to form Al 2 (SO 4 ) 3 .…”
Section: Effect Of Dolostone Application On Soil Phmentioning
confidence: 62%
“…However, soils at this site also contained a relatively high concentration of extractable Al, presumably in the form of aluminum sulfate salts ( Supplemental Table S1), which may indicate the continued oxidation of sulfide ore. The formation of aluminum salts in the 3.6 to 4.5 pH range is consistent with the release of H + ions during oxidation of sulfide ores, counteracting the effect of the dolostone (Xu et al, 2007;Jones et al, 2011). Alternatively, as these soils were exposed to sulfuric acid deposition, there should have been sufficient sulfate available to form Al 2 (SO 4 ) 3 .…”
Section: Effect Of Dolostone Application On Soil Phmentioning
confidence: 62%
“…AAMs immersed in acid water exhibit patterns different from those in deionized water and saltwater. This is mainly because acid water can react with Al and Si ions in the AAM matrix, resulting in the formation of hydroxide complexes such as (Al(OH) 3 ) and (Si(OH) 4 ), oxide complexes such as (Al 2 Si 2 O 5 (OH) 4 ), also known as kaolinite, through hydrolysis reactions, , or even acid–base complexes. These complexes may exhibit characteristic peaks in FTIR spectra, which could be observed in the 900–1150 and 1350–1500 cm –1 regions of the spectrum, depending on their specific coordination environment and bonding configurations.…”
Section: Resultsmentioning
confidence: 99%
“…Active Al in soil, however, exerts important impacts on plant growth. When soil pH falls between 2 and 5, within the buffer range for Al, a large amount of active Al is released (Du & Tian 1996, Huang et al 2005, Xu et al 2007. Although some plants have already been discovered to be Al accumulators (Watanabe et al 1998, Jansen et al 2000, Xie et al 2002, there has been little documentation on rehabilitation or restoration of Al-contaminated soils using these plants on a large scale.…”
mentioning
confidence: 99%