What does the transition from the E horizon typically deposit material into?

The transition from the E horizon typically deposits material into the B horizon. The E horizon, also known as the eluviation horizon, is where leaching occurs, resulting in the removal of minerals and organic material. This process transports these materials downward, leading to accumulation in the B horizon, which is often referred to as the illuviation horizon. The B horizon typically becomes enriched with minerals such as clay, iron, and aluminum, a result of the materials that have leached from the E horizon above.

In soil formation, the B horizon plays a crucial role as it records the history of material transfer from the upper horizons. The E horizon serves primarily as a zone of depletion, while the B horizon accumulates the materials that are washed down, showing the dynamic processes of soil development and nutrient cycling. The relationship between the E and B horizons is significant for understanding soil fertility and management practices in agriculture. The other horizons mentioned do not directly receive the materials deposited from the E horizon in the same manner.