Cargando…

Mineral soil conditioner requirement and ability to adjust soil acidity

Mineral soil conditioners (MSCs) are used to regulate soil acidity and improve soil quality; they are often made in sintering potassium feldspar, limestone, or dolomite, and are alkaline materials rich in silicon, calcium, potassium, and magnesium. The key point of how to apply them into farmlands i...

Descripción completa

Detalles Bibliográficos
Autores principales: Yang, Xiangdong, Feng, Yashuang, Zhang, Xiaohong, Sun, Mingxue, Qiao, Dan, Li, Juan, Li, Xiaoyan
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2020
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7584666/
https://www.ncbi.nlm.nih.gov/pubmed/33097767
http://dx.doi.org/10.1038/s41598-020-75192-5
_version_ 1783599643400077312
author Yang, Xiangdong
Feng, Yashuang
Zhang, Xiaohong
Sun, Mingxue
Qiao, Dan
Li, Juan
Li, Xiaoyan
author_facet Yang, Xiangdong
Feng, Yashuang
Zhang, Xiaohong
Sun, Mingxue
Qiao, Dan
Li, Juan
Li, Xiaoyan
author_sort Yang, Xiangdong
collection PubMed
description Mineral soil conditioners (MSCs) are used to regulate soil acidity and improve soil quality; they are often made in sintering potassium feldspar, limestone, or dolomite, and are alkaline materials rich in silicon, calcium, potassium, and magnesium. The key point of how to apply them into farmlands is their ability to adjust soil acidity and the MSCs requirement (MSC(R)). In this study, inductively coupled plasma-optical emission spectroscopy (ICP-OES) analysis and X-ray diffraction (XRD) were firstly used to determine the elemental and phase compositions of the MSCs in order to establish its equivalent relationship for the depletion of soil activity (H(+)) and its conversion relationship with CaCO(3). Secondly, the soil culture method and the improved Shoemaker Mclean Peatt–Double Buffer (SMP–DB) method were compared using a group of 14 typical acid soils in MSC(R). It is investigated that the MSCs contained four alkali/alkaline earth–metal elements: Ca, Mg, K, and Na in the bound aluminosilicate form (Ca(2)MgAlSi(2)O(7), Ca(3)(SiO(3))(3), KAlSiO(4), and KAlSi(2)O(6)); and the depletion of 2.31 mol of H(+) required 100 g of MSCs and the amount of Si–Ca–K–Mg MSC needed to deplete the same quantity of H(+) was only 0.87 times that of CaCO(3). Based on the calculations by using the SMP-DB method and the soil culture method, the MSC(R) for treating the 14 typical acid soils were in the range of 0.56–8.27 t hm(−2) and 0–10.8 t hm(−2), respectively. Data from both methods were highly correlated with each other and there was a good linear correlation between them, and the equation: [Formula: see text] could be used to calculate the MSCs requirement. The recommended MSC(R) was approximately 4–8, 2–6, and 1–3 t hm(−2) when soil pH < 4.50, 4.50 < pH < 5.50, and pH > 5.50, respectively. The experimental and computational methods established in this study could serve as the scientific basis and theoretical guidance for the production and agricultural use of MSCs.
format Online
Article
Text
id pubmed-7584666
institution National Center for Biotechnology Information
language English
publishDate 2020
publisher Nature Publishing Group UK
record_format MEDLINE/PubMed
spelling pubmed-75846662020-10-27 Mineral soil conditioner requirement and ability to adjust soil acidity Yang, Xiangdong Feng, Yashuang Zhang, Xiaohong Sun, Mingxue Qiao, Dan Li, Juan Li, Xiaoyan Sci Rep Article Mineral soil conditioners (MSCs) are used to regulate soil acidity and improve soil quality; they are often made in sintering potassium feldspar, limestone, or dolomite, and are alkaline materials rich in silicon, calcium, potassium, and magnesium. The key point of how to apply them into farmlands is their ability to adjust soil acidity and the MSCs requirement (MSC(R)). In this study, inductively coupled plasma-optical emission spectroscopy (ICP-OES) analysis and X-ray diffraction (XRD) were firstly used to determine the elemental and phase compositions of the MSCs in order to establish its equivalent relationship for the depletion of soil activity (H(+)) and its conversion relationship with CaCO(3). Secondly, the soil culture method and the improved Shoemaker Mclean Peatt–Double Buffer (SMP–DB) method were compared using a group of 14 typical acid soils in MSC(R). It is investigated that the MSCs contained four alkali/alkaline earth–metal elements: Ca, Mg, K, and Na in the bound aluminosilicate form (Ca(2)MgAlSi(2)O(7), Ca(3)(SiO(3))(3), KAlSiO(4), and KAlSi(2)O(6)); and the depletion of 2.31 mol of H(+) required 100 g of MSCs and the amount of Si–Ca–K–Mg MSC needed to deplete the same quantity of H(+) was only 0.87 times that of CaCO(3). Based on the calculations by using the SMP-DB method and the soil culture method, the MSC(R) for treating the 14 typical acid soils were in the range of 0.56–8.27 t hm(−2) and 0–10.8 t hm(−2), respectively. Data from both methods were highly correlated with each other and there was a good linear correlation between them, and the equation: [Formula: see text] could be used to calculate the MSCs requirement. The recommended MSC(R) was approximately 4–8, 2–6, and 1–3 t hm(−2) when soil pH < 4.50, 4.50 < pH < 5.50, and pH > 5.50, respectively. The experimental and computational methods established in this study could serve as the scientific basis and theoretical guidance for the production and agricultural use of MSCs. Nature Publishing Group UK 2020-10-23 /pmc/articles/PMC7584666/ /pubmed/33097767 http://dx.doi.org/10.1038/s41598-020-75192-5 Text en © The Author(s) 2020 Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article's Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article's Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by/4.0/.
spellingShingle Article
Yang, Xiangdong
Feng, Yashuang
Zhang, Xiaohong
Sun, Mingxue
Qiao, Dan
Li, Juan
Li, Xiaoyan
Mineral soil conditioner requirement and ability to adjust soil acidity
title Mineral soil conditioner requirement and ability to adjust soil acidity
title_full Mineral soil conditioner requirement and ability to adjust soil acidity
title_fullStr Mineral soil conditioner requirement and ability to adjust soil acidity
title_full_unstemmed Mineral soil conditioner requirement and ability to adjust soil acidity
title_short Mineral soil conditioner requirement and ability to adjust soil acidity
title_sort mineral soil conditioner requirement and ability to adjust soil acidity
topic Article
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7584666/
https://www.ncbi.nlm.nih.gov/pubmed/33097767
http://dx.doi.org/10.1038/s41598-020-75192-5
work_keys_str_mv AT yangxiangdong mineralsoilconditionerrequirementandabilitytoadjustsoilacidity
AT fengyashuang mineralsoilconditionerrequirementandabilitytoadjustsoilacidity
AT zhangxiaohong mineralsoilconditionerrequirementandabilitytoadjustsoilacidity
AT sunmingxue mineralsoilconditionerrequirementandabilitytoadjustsoilacidity
AT qiaodan mineralsoilconditionerrequirementandabilitytoadjustsoilacidity
AT lijuan mineralsoilconditionerrequirementandabilitytoadjustsoilacidity
AT lixiaoyan mineralsoilconditionerrequirementandabilitytoadjustsoilacidity