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<p><a href="page.php?w=organic_matter">organic matter</a> compounds, has a crucial role in the formation and stability of soil aggregates. <a href="page.php?w=Calcium">Calcium</a> can exchange with <a href="page.php?w=sodium">sodium</a> on exchange sites. This, in turn, reduces soil particle dispersion, <a href="page.php?w=Soil_crust">surface crusting</a>, and aggregate <a href="page.php?w=Slaking_%28geology%29">slaking</a> associated with <a href="page.php?w=Sodic_soil">sodic</a> soils and indirectly increase aggregate stability.</p>

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