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Soil fertility

Mineral weathering and silicon uptake by rice plants promote carbon storage in paddy fields

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Pages 162-170 | Received 01 Mar 2020, Accepted 17 Jan 2021, Published online: 21 Apr 2021

Figures & data

Table 1. Yield, potassium (K) and silicon (Si) uptake and balance (annual and average) in forage rice cultivars

Figure 1. Temporal changes in aluminum and organic carbon contents of extracts from soils by a 5-step sequential procedure. (a) Al contents extracted by 0.5 M CuCl2 solution (AlCu) and 0.1 M Na-pyrophosphate solution (Alp). Alp in FRC-soil (r = 0.73, P = 0.011, Increase rate (Δ) = 57 mg Al kg−1 year-1), AlCu in FRC-soil (r = 0.83 P = 0.002, Δ = 16 mg Al kg−1 year−1), and AlCu in ERC-soil (r = 0.88, P = 0.001, Δ = 13 mg Al kg-1 year-1) increased linearly with time. (b) Organic carbon content extracted by 0.1 M Na-pyrophosphate solution (Cp). Cp in FRC-soil (r = 0.65 P = 0.029, Δ = 73 mg C kg-1 year-1) increased linearly with time

Figure 1. Temporal changes in aluminum and organic carbon contents of extracts from soils by a 5-step sequential procedure. (a) Al contents extracted by 0.5 M CuCl2 solution (AlCu) and 0.1 M Na-pyrophosphate solution (Alp). Alp in FRC-soil (r = 0.73, P = 0.011, Increase rate (Δ) = 57 mg Al kg−1 year-1), AlCu in FRC-soil (r = 0.83 P = 0.002, Δ = 16 mg Al kg−1 year−1), and AlCu in ERC-soil (r = 0.88, P = 0.001, Δ = 13 mg Al kg-1 year-1) increased linearly with time. (b) Organic carbon content extracted by 0.1 M Na-pyrophosphate solution (Cp). Cp in FRC-soil (r = 0.65 P = 0.029, Δ = 73 mg C kg-1 year-1) increased linearly with time

Table 2. Yield, potassium (K) and silicon (Si) uptake and balance (annual and average) in edible rice cultivars

Figure 2. Schematic chemical reaction of weathering process of primary minerals by root surface cell wall (CW) of plants and nutritional K and Si (a), or only K (b) are taken up by the plants. Solubilized active Al reacts with organic compounds to form persistent soil storage carbon

Figure 2. Schematic chemical reaction of weathering process of primary minerals by root surface cell wall (CW) of plants and nutritional K and Si (a), or only K (b) are taken up by the plants. Solubilized active Al reacts with organic compounds to form persistent soil storage carbon

Table 3. Organic acids exuded from the roots of 5 plant species

Table 4. Elements released (K, Si, Al) by “contact reactions” between plant roots and soils or minerals (orthoclase, obsidian, kaolinite)

Appendix 1. Exchangeable potassium (K) and non-exchangeable K contents in FRC-soils

Appendix 2. Exchangeable potassium (K) and non-exchangeable K contents in ERC- soils

Appendix 3. Extractable aluminum contents by 5-sequential extraction in FRC- soils

Appendix 4. Extractable aluminum contents by 5-sequential extraction in ERC- soils

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