In the semi-arid area of western Liaoning Province and the semi-humid area of eastern of Liaoning Province
field observations showed that the temperature in a mining area was higher than CK in summer by 2℃ and 7℃ respectively
but below CK in the spring and the autumn. In the spring and autumn
the moisture content of the mining residue pile was 6% and 11% respectively
while the moisture content of the mining residue pile in the arid period was at wilting point or lower. Evaporation from mining area increased by 1-5mm compared with CK
but the humidity of mining area was much lower than CK.
Windbreak efficiency of typical windbreak and sand-fixation shelterbelts in western Heilongjiang Province
Effects of post-snowmelt intermittent rainfall on water infiltration on loess slopes of Ili Region
Spatiotemporal evolution characteristics and influencing factors of cultivated land use transition on Loess Plateau in east Gansu Province
Ecological security evaluation and prediction in Xizang Autonomous Region
Mechanical characteristics of root system of dominant herbaceous plants and shear strength of root-soil composites in Jialangpute landslide area of Yili valley