The global magnitude (Pg) of soil organic carbon (SOC) is 677 to 0.3‐m, 993 to 0.5‐m, and
1,505 to 1‐m depth. Thus,~ 55% of SOC to 1‐m lies below 0.3‐m depth. Soils of …

During the last few decades, many case studies focused on the dynamics of fluvial systems
in response to hillslope erosion, land-use impact, and climate changes. This paper will …

Sediment deposition in floodplains is an essential part of the sediment dynamics of a
catchment. These sediment dynamics can vary largely on a Holocene time scale under the …

Investigators have studied past environmental change in the Eastern Mediterranean region
from a number of perspectives. While climate reconstructions and palynological research …

Luminescence dating determines the last exposure to light of quartz and feldspar mineral
grains and thus the time a sediment was laid down. Prerequisite is that the sediment grains …

This paper presents the results of 40years of research on the gully system in the Doły
Podmularskie catchment (0.35 km² in size), which is situated in the south-western part of the …

Humans have greatly impacted the processes and intensities of erosion, sediment transport
and storage since the introduction of agriculture. In many regions around the world …

An increasing number of studies have indicated that soil erosion, sediment redistribution
and water discharge during the Holocene have varied greatly under influence of …

A Holocene sediment budget was constructed for the 758 km2 Dijle catchment in the
Belgian loess belt, in order to understand long-term sediment dynamics. Hillslope sediment …

This study presents a Holocene sediment budget for the Nethen catchment, a typical river
catchment (55 km2) in the Belgian loess belt. Soil erosion and hillslope sediment storage …