What typically happens to the organic matter content in well-aerated coarse textured soils?

In well-aerated coarse textured soils, the organic matter content typically disappears rapidly. This occurs because coarse textured soils, such as sand or loamy sand, have larger particle sizes which result in higher drainage and aeration. While good aeration is beneficial for root development and microbial activity, it also leads to more rapid decomposition of organic matter.

Microorganisms in these well-aerated environments break down organic materials more quickly, as they have access to oxygen, which supports aerobic decomposition processes. As a result, the organic matter doesn't accumulate but tends to get degraded faster, leading to a depletion in organic content over time. This is contrasted with finer textured soils, where organic matter can be retained longer due to slower decomposition rates and better moisture retention capabilities. Hence, the rapid depletion of organic matter in well-aerated coarse textured soils is the correct point to highlight.