Formation causes and recovery of the “Black Soil Type” degraded alpine grassland in Qinghai-Tibetan Plateau

Author:

Shang Zhanhuan,Long Ruijun

Publisher

Springer Science and Business Media LLC

Subject

Agronomy and Crop Science

Reference74 articles.

1. Bai W Q, Zhang Y L, Xie G D, Shen Z X (2002). Analysis of formation causes of grassland degradation in Maduo County in the source region of Yellow River. Chinese Journal of Applied Ecology, 13(7): 823–826 (in Chinese)

2. Brockway D G, Gatewood R G, Paris R B (2002). Restoring grassland savannas from degraded pinyon-juniper woodlands: Effects of mechanical overstory reduction and slash treatment alternatives. Journal Environment Management, 64: 179–197

3. Cao W B, Wan L, Zhou X, Hu F S, Li Z M, Liang S H (2003). A study of the geological environmental of suprapermafrost water in the headwater area of the Yellow River. Hydrogeology and Engineering Geology, 30(6): 6–10 (in Chinese)

4. Chen G C, Huang Z W, Lu X F, Peng M (2002). Characteristics of wetland and its conservation in the Qinghai Plateau. Journal of Glaciology and Geocryology, 24(3): 254–259 (in Chinese)

5. Deng Z F, Xie X L, Wang Q J, Zhou X M (2001). Study on reproduction strategies of Kobresia tiberica population on alpine meadow. Chinese Journal of Applied and Environmental Biology, 7(4): 332–334 (in Chinese)

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