For soils that have a water retention layer consisting of lithic or paralithic fragments, what should be done?

In this context, when encountering a soil with a water retention layer made up of lithic or paralithic fragments, the appropriate action is to stop at that layer. Lithic and paralithic fragments typically indicate a hard or rocky layer that can significantly impact water movement and root penetration.

Stopping at this layer is essential because it serves as a boundary that may prevent roots from growing deeper and limit water infiltration into the soil beneath. This boundary causes the soil above to retain moisture, but it also hinders drainage and can lead to saturation during wet periods. Recognizing this layer allows for a better understanding of the soil's characteristics and how they affect plant growth and moisture dynamics, which is crucial for accurate soil assessment and management decisions.

Other choices do not appropriately address the implications of encountering a lithic or paralithic layer. Continuing to measure depth through these layers disregards the significant physical barriers they present. Counting this layer as valuable for moisture retention is misleading because while it can hold water, it also limits drainage, making it less beneficial for plant roots. Lastly, solely considering roots in the assessment would overlook other critical soil properties influenced by the presence of these fragments.