2022
DOI: 10.31545/intagr/148101
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Effect of mineral and organic additions on soil microbial composition

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Cited by 10 publications
(8 citation statements)
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“…It was proven that copper-ion-exchanged zeolite X, using a 0.05 M solution of copper(II) nitrate and a proton form of zeolite X, displayed improved adsorption capacities toward phosphate ions in comparison with parent zeolite NaX–FA by 20-fold and 8-fold, respectively. The application of zeolites in mineral–organic mixtures as fertilizers was also widely investigated, both before and after in vivo experiments with plants, to investigate their effect on soil microbial composition [ 26 ] and their effect on both plant growth and the translocation of heavy metals from soil to plant tissues [ 27 ].…”
Section: Introductionmentioning
confidence: 99%
“…It was proven that copper-ion-exchanged zeolite X, using a 0.05 M solution of copper(II) nitrate and a proton form of zeolite X, displayed improved adsorption capacities toward phosphate ions in comparison with parent zeolite NaX–FA by 20-fold and 8-fold, respectively. The application of zeolites in mineral–organic mixtures as fertilizers was also widely investigated, both before and after in vivo experiments with plants, to investigate their effect on soil microbial composition [ 26 ] and their effect on both plant growth and the translocation of heavy metals from soil to plant tissues [ 27 ].…”
Section: Introductionmentioning
confidence: 99%
“…The DhA in soils are usually the most sensitive indicator of environmental changes, and their activities are always affected by soil conditions through shifting the synthesis and structure of local microorganisms 39 . It was also evidenced that zeolites, due to their high porosity and well-developed specific surface area, can improve the soil’s microbial activity 26 , 27 , 40 . The DhA in amended soils was lower compared to the control, except for C9L6.…”
Section: Discussionmentioning
confidence: 99%
“…These fluctuations will be manifested through the intensity of water distribution and temperature increases. In recent years, a lack of precipitation has been the restraining factor in plant growth, yields, and in the subsequent decomposition of crop residues in the soil (Katerji et al, 2004;Von Lützow et al, 2006;Peña-Gallardo et al, 2019;Mitchell-Forsytk et al, 2021;Wolny-Koładka et al, 2022). Disturbances such as these cause a deterioration in the physical properties of the soil through a lack of soil organic matter and also result in the degradation of the soil structure which is induced by compaction (Nimmo, 2013;Hábová et al, 2016).…”
Section: Introductionmentioning
confidence: 99%