Soil Moisture Characteristics of Different Vegetations in Northern of Ziwuling
Zhao Shi
Abstract
Zhao Shi
Abstract
The soil water characteristics of different vegetations in the northern loess area of ziwuling were studied. The results show that:there was s high power function correlation between the soil moisture and the potential of soil water. The mathematical model is:θ=aS b. The value a and soil water content of different vegetations were ranged in order from higher ones to lower ones as follow:Quercus laotungensis,Betula platyphylla Suk.,Populus davidiana Dode.,Sophora viciifolia,Artemisia sacrorum, Bothriochloa ischaemum and abandoned land at a same soil potential. At the low soil potential range, the difference of 0~20 cm soil water content in vegetations was very distinctly, the soil water content of arbor forest was the highest and shrub forestgrasslad abandoned land; in the 20~50 cm soil, the difference of water content in vegetations was reduced with the raising of soil potential. At the middle soil potential range, the 0~20 cm soil water content in arbor forest was the best, in grassland was over shrub forest; in the 20~50 cm, the tend of soil water content was as same as in 0~20 cm soil. The types of vegetation affect soil water characteristics by increasing the soil organic matter, improving the soil construction, receding soil bulk density and enhancing the soil porosity.
OpenAlex reports 5 citations for this work. Citation counts describe recorded attention and do not establish research quality.
A contribution statement is not available in the OpenAlex record.
Method details are not available in the OpenAlex metadata.
Findings are not separately available in the OpenAlex metadata.
Limitations are not available in the OpenAlex metadata.
Application details are not available in the OpenAlex metadata.
The soil water characteristics of different vegetations in the northern loess area of ziwuling were studied. The results show that:there was s high power function correlation between the soil moisture and the potential of soil water. The mathematical model is:θ=aS b. The value a and soil water content of different vegetations were ranged in order from higher ones to lower ones as follow:Quercus laotungensis,Betula platyphylla Suk.,Populus davidiana Dode.,Sophora viciifolia,Artemisia sacrorum, Bothriochloa ischaemum and abandoned land at a same soil potential. At the low soil potential range, the difference of 0~20 cm soil water content in vegetations was very distinctly, the soil water content of arbor forest was the highest and shrub forestgrasslad abandoned land; in the 20~50 cm soil, the difference of water content in vegetations was reduced with the raising of soil potential. At the middle soil potential range, the 0~20 cm soil water content in arbor forest was the best, in grassland was over shrub forest; in the 20~50 cm, the tend of soil water content was as same as in 0~20 cm soil. The types of vegetation affect soil water characteristics by increasing the soil organic matter, improving the soil construction, receding soil bulk density and enhancing the soil porosity.
Key concepts: Environmental science, Water content, Soil water, Shrub, Soil science, Bulk density, Vegetation (pathology), Agronomy