The effect of calcium silicate and ground magnesium limestone (GML) on the chemical characteristics of acid sulfate soil.


Journal

PloS one
ISSN: 1932-6203
Titre abrégé: PLoS One
Pays: United States
ID NLM: 101285081

Informations de publication

Date de publication:
2023
Historique:
received: 02 03 2022
accepted: 14 08 2023
medline: 18 9 2023
pubmed: 15 9 2023
entrez: 15 9 2023
Statut: epublish

Résumé

Acid sulfate soil characterized by pyrite (FeS2) which produces high acidity (soil pH < 3.5) and release high amount of Al3+ and Fe2+. Application of 4 t ha-1 Ground Magnesium Limestone (GML), is a common rate used for acid sulfate soil by the rice farmers in Malaysia. Therefore, this study was conducted to evaluate the integral effect of ground magnesium limestone (GML) and calcium silicate and to determine the optimal combination on acid sulfate soils in Malaysia. The acid sulfate soils were incubated under the submerged condition for 120 days with GML (0, 2, 4, 6 t ha-1) in combination with calcium silicate (0, 1, 2, 3 t ha-1) arranged in a Completely Randomized Design (CRD). The soil was sampled after 30, 60, 90 and 120 days of incubation and analyzed for soil pH, exchangeable Al, Ca, Mg, K and available Si. A total of 2 out of 16 combinations met the desired soil requirement for rice cultivation. The desired chemical soil characteristics for rice cultivation are soil pH > 4, exchangeable Al < 2 cmolc Kg-1, exchangeable Ca > 2 cmolc kg-1, exchangeable Mg > 1 cmolc kg-1 and Si content > 43 mg kg-1. The combinations are i) 2 t ha-1 calcium silicate + 2 t ha-1 GML, and ii) 3 t ha-1 calcium silicate + 2 t ha-1 GML, respectively. These combination rates met the desired requirement of soil chemical characteristics for rice cultivation. Soil acidity was reduced by a gradual release of Ca2+ and SiO32- from calcium silicate continuously filling the exchange sites and reducing the potential of extra (free) H+ availability in the soil system. Combination of calcium silicate and GML, shows the ameliorative effect with; i) release of Ca, ii) binding of Al3+ making it inert Al-hydroxides and, iii) bind H+ to produce water molecules.

Identifiants

pubmed: 37713375
doi: 10.1371/journal.pone.0290703
pii: PONE-D-22-06213
pmc: PMC10503729
doi:

Substances chimiques

calcium silicate S4255P4G5M
Calcium Carbonate H0G9379FGK
Magnesium I38ZP9992A
Sulfates 0
Soil 0
Sulfur Oxides 0

Types de publication

Journal Article

Langues

eng

Sous-ensembles de citation

IM

Pagination

e0290703

Informations de copyright

Copyright: © 2023 Azman et al. This is an open access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.

Déclaration de conflit d'intérêts

The authors have declared that no competing interests exist.

Références

J Plant Physiol. 2006 Jul;163(8):847-55
pubmed: 16777532
Environ Pollut. 2007 May;147(2):422-8
pubmed: 16996179

Auteurs

Elisa Azura Azman (EA)

Faculty of Agriculture, Department of Crop Science, Universiti Putra Malaysia, Serdang, Malaysia.

Roslan Ismail (R)

Faculty of Agriculture, Department of Land Management, Universiti Putra Malaysia, Serdang, Malaysia.

Seishi Ninomiya (S)

Department of Global Agriculture, Graduate School of Agricultural and Life Sciences, The University of Tokyo, Tokyo, Japan.

Shamshuddin Jusop (S)

Faculty of Agriculture, Department of Land Management, Universiti Putra Malaysia, Serdang, Malaysia.

Uraiwan Tongkaemkaew (U)

Faculty of Technology and Community Development, Department of Plant Science, Thaksin University, Phatthalung, Thailand.

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Classifications MeSH