Wenqiang Xu

The relationship between soil, climate and forest development in the mid-mountain zone of the Sangong River watershed in the northern Tianshan Mountains, China

The mountainous forests in arid regions, being sensitive to climate change, are one of the key research topics related to the mechanism of interaction between climate and the terrestrial ecosystem. In this study, the spatial distribution of a mid-mountain forest and its environmental factors were investigated by using a combination of remote sensing technology, field survey, climate indices and soil nutrient analysis in the Sangong River watershed of the northern Tianshan Mountains. The forest (Picea schrenkiana) was distributed between 1,510 and 2,720 m asl. Tree height and diameter at breast height (DBH) exhibited a bi-modal pattern with increasing elevation, and rested at 2,450 and 2,250 m asl, respectively. The two maxima of DBH appeared at 2,000 and 2,550 m asl, and the taller trees were observed at 2,100 and 2,600 m asl. For the annual mean temperature, the difference was approximately 5.8°C between the lowest and the highest limits of the forest, and the average decreasing rates per hundred meters were 0.49°C and 0.55°C with increasing altitude between 1,500 and 2,000 m asl and above 2,000 m asl, respectively. The annual precipitation in the forest zone first increased and then decreased with the increase of altitude, and the maximum value was at 2,000 m asl. For per hundred meters, the annual precipitation increased with the rate of 31 mm between 1,500 and 2,000 m asl and decreased by 7.8 mm above 2,000 m asl. The SOM, TN and TP were high between 2,000 and 2,700 m asl and low at the lower and upper forest limits. The minimum CaCO3 concentration, pH value and EC coincided with the maximum precipitation belt at 2,000 m asl. The SOM, TN and TP were high in the topsoil (0–10 cm) and differed significantly from the values observed in the deep soil layers (>10 cm). The soil nutrients exhibited spatial heterogeneity and higher aggregation in the topsoil. In conclusion, soil and climate are closely related to each other, working synergistically to determine the development and spatial distribution of the mid-mountain forest in the study area. The order of the importance of environmental factors to forest development in this study is as follows: soil nutrients>precipitation>elevation>temperature.

Evaluation of land use change degree and ecological security in the Manas River Basin, Xinjiang, China

In this paper, we evaluate the extent of land use change and ecological security grades in the Manas River Basin, on the northern slopes of the Tianshan Mountains, from 1989–2002. Surveys were performed using Remote Sensing (RS) and Geographic Information System (GIS) means, and the relationship between land use change and ecological security was analyzed. The results are as follows: (i) the degree of land use change steadily increased in the Manas River Basin, and overall land use was in a state of development; (ii) From 1989–2002, the ecological security of the drainage basin generally improved somewhat, but deteriorated subsequently in some regions; (iii) the ecological security grade increased in regions with land use composite change extent values of 18–100, and ecological security grade improved from moderate warning in 1989 to early warning in 2002; and (iv) the cumulative areas of regions with relatively secure, and early-warning ecological security grade were ranked by land use degree in the order, V > IV > I > VI > III > II, showing that that regions with land use degree V (woodlands and grasslands) were important areas for ecological restoration and regeneration in this drainage basin, and that it was difficult to improve the ecological environment on sandy soils. We suggest that ecological security grades can be improved by increasing land use degree in regions where it is low.