investigation of desertification trend needs understanding of phenomena creating changes singly or action and reaction together in the manner that these changes were ended up in land degradation. in investigation of pedological criterion onland degradation in quaternary rock units, first, a part of the rude-shoor watershed area was selected. after distinguishing target area, maps of slope class...

Remote sensing (RS) has revolutionized field data collection processes and provided timely spatially consistent acquisition of on the terrestrial landscape properties. This research paper investigates relationship between Wind Erosion (WE) Sensing techniques. By examining, analyzing, reviewing recent studies utilizing RS, we underscore importance wind erosion by exploring indicators that influe...

The objectives of this present study were to analyses soils and find out some soil quality properties check relationship between compaction, crust formation erodibility - K the with organic carbon (SOC) amount in surface (0-20 cm) subsurface (20-40 affected by long-time continuous cultivation under sub-humid environmental condition. research comes showed that formation, is highly significantly ...

Redistribution of soil, nutrients, and contaminants is often driven by wind erosion in semiarid shrublands. Wind erosion depends on wind velocity (particularly during episodic, high-velocity winds) and on vegetation, which is generally sparse and spatially heterogeneous in semiarid ecosystems. Further, the vegetation cover can be rapidly and greatly altered due to disturbances, particularly fir...

Sodium accumulating playas (also termed sodic or natric playas) are typically covered by polygonal crusts with different pattern characteristics, but little is known about the short-term (hours) dynamics of these patterns or how pore water may respond to or drive changing salt crust patterning and surface roughness. It is important to understand these interactions because playa-crust surface po...