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Mineral-dependent physicochemical regimes govern the adsorption of soil viral communities
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DOI：10.1016/j.apsoil.2026.107235.png)
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Abstract
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• The fate of soil viruses is a complex interplay of mineral and viral properties. • The pH dependence of adsorption reverses with mineral surface charge. • Ionic bridging operates as a vital supplemental mechanism to electrostatic control. • Viral community diversity contributes to the contrasting virus-mineral interaction.
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