The report provides documented scientific data on soil erosion, soil organic carbon change, soil biodiversity changes, soil acidification, soil compaction, soil sealing, soil salinization and sodification, soil contamination, soil nutrient changes and water logging.
The quality of organic carbon data of the soils depends on sampling methods, the kind of vegetation, and the method of soil analysis performed in the laboratory.
A mass of data on the environment, soils, flora, fauna, land use, settlement patterns, and artifactual history of the entire region has become available through geomorphologic, hydrologic, and archaeological surveys.
This paper provides data on the landforms, soils, and sediments within a unique northern Michigan landscape known as the Grayling Fingers, and evaluates these data to develop various scenarios for the geomorphic development of this region.
Nave et al. [28] used a meta-analysis of 432 data sets on the soil-C response ratio to show that a clear-cutting leads, on average, to an 8 % reduction in soil carbon.
Nave et al. [ 28] used a meta-analysis of 432 data sets on the soil-C response ratio to show that a clear-cutting leads, on average, to an 8 % reduction in soil carbon.
A method is proposed for using data on the distribution of soil types to map the variable preservation capacities of soil for different materials.
For the first time, data on the structure of soil cover in the dry steppe zone during Sarmatian times (AD 1) were obtained.
While this is well recognised there is a lack of data on the variability of soil temperature at the hillslope and catchment scale.
