Two human factors affecting water balance in desert oases of northwest China;

Zonation of desert and sandy desertification land in North China based on remote sensing technology;

Desert and controlling of aeolian disaster in Xinjiang.;

This article pointed out that the distributing pattern of Chinese desert and desertification is V shapesd, and the Qinghai-Tibet plateau uplift may be the main factor to this pattern.

Sodium ion contents of desert plants irrigation with waster water of paper making in different years and in different vegetal parts were measured.

Temperate desert plants always grow in the high temperature, arid and water deficit environment throughout a year.

In desert area of Jing-Yu Gas Pipeline of Second Shan-Jing Pipeline Project, soil layers belong tofine silty sand and have very low bearing capacity.

The results from remote sensor monitoring and field survey show that aeolian desertification process in the study area can be distributed into two stages: the developing stage from late 1980s to 2000,and the reversing stage form 2000 to 2006.

The aeolian desertification is a land degradation characterized by wind erosion mainly resulted from the excessive human activities in arid, semiarid and part of sub-humid regions in Northern Chian.

Deterioration of climate conditions,continuous desiccation for instance,can lead to aeolian desertification,and aeolian desertification can give a negative reaction to climate change through biogeophysical feedback,releasing more dust aerosol and increasing greenhouse gases concentration.