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example, if the site is in a river valley, it is reasonable to expect that the site will reflect fluvial dynamics and features in the landforms, sediments, and soils of the area. The location of the site within the river valley e.g., headwaters vs. delta can further refine preliminary expectations. Headwater fluvial sediments, and the soils that formed in them, may be expected to contain more, larger, and less rounded coarse fragments, be somewhat less well sorted, and have less contrasting sediment strata than fluvial sediments in a delta. In addition, general conditions and dynamics for a water table might be anticipated e.g., gaining stream vs. losing stream based on the prevailing climate. A preliminary model can provide a tentative framework in which scientists can begin to efficiently investigate, understand, and give order to a diverse natural world. In the digital world, this now includes considerable pre-mapping, based primarily upon improved, detailed digital elevation models and existing information . Preliminary soil-landscape models are helpful. The adage “If I hadn’t known about it, I wouldn’t have recognized it” is a relevant and practical truth. The more one understands a natural system, the easier it becomes to recognize the physical expressions of those systems. This chapter describes information that is recorded about the overall setting and site features for a soil. This information includes the physiographic and landscape setting, geomorphological characteristics, and other information specific to the area where the soil is described. The setting and site often include information on drainage pattern, parent material, bedrock, erosion, land cover, and relationships to vegetation communities. Detailed information about describing soil profiles is provided in chapter . Reduced soil erosion, increased nitrogen retention, greater water uptake efficiency and enhanced carbon sequestration represent improved ecosystem functions, made possible in part by deep and extensive root systems of perennial crops Figure 8. In research on land degradation, climate and climate variability are often intrinsic factors. The role of climate change, however, is less articulated. Depending on what conceptual framework is used, climate change is understood either as a process or a driver of land degradation, and sometimes both. In summary, agriculture and clearing of land for food and wood products have been the main drivers of land degradation for millennia . This does not mean, however, that agriculture and forestry always cause land degradation ; sustainable management is possible but not always practised . Reasons for this are primarily economic, political and social. Human activity altering the vegetation of an area is perhaps the biggest human factor contributing to erosion. Trees and plants hold soil in place. When people cut down forests or plow up grasses for agriculture and development, the soil is more vulnerable to washing or blowing away. Landslides become more common. Water

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