The natural environments in the semiarid regions of the Chinese Loess Plateau (CLP) are fragile due to the serious soil erosion and the weak ecological services of the plants. To ascertain and then evaluate a sustainable land-use pattern in these regions, we selected six typical land-use patterns (i.e., a farmland, a natural grassland, a homogeneous shrubland (S), a mix of shrubland and cultivated grassland (S–Alf), a mix of shrubland and orchard (S–O) and a mix of shrubland and grassland (S–G)) on the plateau and then measured the soil water, related soil properties and plant root indices to a depth of 1800 cm. We also measured the aboveground net primary productivities (ANPPs). The mean soil water content (SWC) within th...
Changes in land use type can lead to variations in soil water characteristics. The objective of this...
A dried soil layer (DSL) formed in the soil profile is a typical indication of soil drought caused b...
Knowledge of soil moisture spatial variation with land use along the precipitation gradient is neces...
The natural environments in the semiarid regions of the Chinese Loess Plateau (CLP) are fragile due ...
In order to reduce soil erosion and desertification, the Sloping Land Conversion Program has been co...
In order to reduce soil erosion and desertification, the Sloping Land Conversion Program has been co...
The Loess Plateau has been suffering from serious soil erosion for a long time, which originated in ...
China's Sloping Land Conversion Programme (SLCP) improves the vegetation at the expense of a lot of ...
Vegetation restoration is helpful in preventing soil erosion but aggravates water scarcity, thus res...
The water-wind crisscross region of the Loess Plateau in China is comprised of 17.8 million hectares...
Abstract There is an urgent need to study soil water resources and eco-hydrological characteristics ...
The water-wind crisscross region of the Loess Plateau in China is comprised of 17.8 million hectares...
The water-wind crisscross region of the Loess Plateau in China is comprised of 17.8 million hectares...
The water-wind crisscross region of the Loess Plateau in China is comprised of 17.8 million hectares...
Changes in land use type can lead to variations in soil water characteristics. The objective of this...
Changes in land use type can lead to variations in soil water characteristics. The objective of this...
A dried soil layer (DSL) formed in the soil profile is a typical indication of soil drought caused b...
Knowledge of soil moisture spatial variation with land use along the precipitation gradient is neces...
The natural environments in the semiarid regions of the Chinese Loess Plateau (CLP) are fragile due ...
In order to reduce soil erosion and desertification, the Sloping Land Conversion Program has been co...
In order to reduce soil erosion and desertification, the Sloping Land Conversion Program has been co...
The Loess Plateau has been suffering from serious soil erosion for a long time, which originated in ...
China's Sloping Land Conversion Programme (SLCP) improves the vegetation at the expense of a lot of ...
Vegetation restoration is helpful in preventing soil erosion but aggravates water scarcity, thus res...
The water-wind crisscross region of the Loess Plateau in China is comprised of 17.8 million hectares...
Abstract There is an urgent need to study soil water resources and eco-hydrological characteristics ...
The water-wind crisscross region of the Loess Plateau in China is comprised of 17.8 million hectares...
The water-wind crisscross region of the Loess Plateau in China is comprised of 17.8 million hectares...
The water-wind crisscross region of the Loess Plateau in China is comprised of 17.8 million hectares...
Changes in land use type can lead to variations in soil water characteristics. The objective of this...
Changes in land use type can lead to variations in soil water characteristics. The objective of this...
A dried soil layer (DSL) formed in the soil profile is a typical indication of soil drought caused b...
Knowledge of soil moisture spatial variation with land use along the precipitation gradient is neces...