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Measuring and Mapping Patterns of Soil Erosion and Deposition Related to Soil Carbonate Concentrations Under Agricultural Management
Published on: September 12, 2017
Mineral soil conditioner requirement and ability to adjust soil acidity
Xiangdong Yang1, Yashuang Feng2, Xiaohong Zhang2
1Key Laboratory of Plant Nutrition and Fertilizer, Ministry of Agriculture and Rural Affairs/Institute of Agricultural Resources and Regional Planning, Chinese Academy of Agricultural Sciences, Beijing, 100081, China.
Mineral soil conditioners (MSCs) effectively regulate soil acidity by neutralizing H+ ions. This study establishes a method to determine the optimal MSCs requirement for agricultural application, offering guidance for soil quality improvement.
Area of Science:
- Soil Science
- Agricultural Chemistry
- Mineralogy
Background:
- Mineral soil conditioners (MSCs) are alkaline materials used to improve soil quality and regulate soil acidity.
- MSCs are typically composed of silicon, calcium, potassium, and magnesium, often derived from sintering potassium feldspar, limestone, or dolomite.
- Determining the precise application rate (MSCs requirement, MSCR) for effective soil amendment is crucial.
Purpose of the Study:
- To establish an equivalent relationship for the depletion of soil activity (H+) and its conversion with CaCO3 using MSCs.
- To compare the soil culture method and the improved Shoemaker Mclean Peatt-Double Buffer (SMP-DB) method for determining MSCR.
- To provide a scientific basis and theoretical guidance for the production and agricultural use of MSCs.
Main Methods:
- Inductively coupled plasma-optical emission spectroscopy (ICP-OES) and X-ray diffraction (XRD) were employed to analyze the elemental and phase compositions of MSCs.
- The study utilized a soil culture method and the improved SMP-DB method to assess MSCR across 14 typical acid soils.
- Elemental and phase composition analysis determined the binding forms of alkali/alkaline earth-metal elements within the MSCs.
Main Results:
- MSCs contain Ca, Mg, K, and Na in bound aluminosilicate forms, such as Ca2MgAlSi2O7, Ca3(SiO3)3, KAlSiO4, and KAlSi2O6.
- 100 g of MSCs can deplete 2.31 mol of H+, and the amount of MSCs needed is 0.87 times that of CaCO3 for equivalent H+ depletion.
- Calculated MSCR ranged from 0.56-8.27 t hm-2 (soil culture) and 0-10.8 t hm-2 (SMP-DB), showing a strong linear correlation between the two methods.
Conclusions:
- A reliable formula was derived from the correlated data to calculate the MSCs requirement.
- Recommended MSCR varies with soil pH: 4-8 t hm-2 for pH < 4.50, 2-6 t hm-2 for 4.50 < pH < 5.50, and 1-3 t hm-2 for pH > 5.50.
- The established experimental and computational methods provide a scientific foundation for optimizing MSC application in agriculture.
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