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干旱区科学  2013, Vol. 5 Issue (3): 354-365    DOI: 10.1007/s40333-013-0182-y
  学术论文 本期目录 | 过刊浏览 | 高级检索 |
Modeling grassland net primary productivity and water-use efficiency along an elevational gradient of the Northern Tianshan Mountains
QiFei HAN1,2, GePing LUO1*, ChaoFan LI1,2, Hui YE1,2, YaoLiang CHEN1,2
1 State Key Laboratory of Desert and Oasis Ecology, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, China;
2 University of Chinese Academy of Sciences, Beijing 100049, China
Modeling grassland net primary productivity and water-use efficiency along an elevational gradient of the Northern Tianshan Mountains
QiFei HAN1,2, GePing LUO1*, ChaoFan LI1,2, Hui YE1,2, YaoLiang CHEN1,2
1 State Key Laboratory of Desert and Oasis Ecology, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, China;
2 University of Chinese Academy of Sciences, Beijing 100049, China
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摘要 Mountainous ecosystems are considered highly sensitive and vulnerable to natural disasters and climatic changes. Therefore, quantifying the effects of elevation on grassland productivity to understand ecosystem-climate interactions is vital for mountainous ecosystems. Water-use efficiency (WUE) provides a useful index for understanding the metabolism of terrestrial ecosystems as well as for evaluating the degradation of grasslands. This paper explored net primary productivity (NPP) and WUE in grasslands along an elevational gradient ranging from 400 to 3,400 m asl in the northern Tianshan Mountains–southern Junggar Basin (TMJB), Xinjiang of China, using the Biome-BGC model. The results showed that: 1) the NPP increased by 0.05 g C/(m2×a) with every increase of 1-m elevation, reached the maximum at the mid-high elevation (1,600 m asl), and then decreased by 0.06 g C/(m2×a) per 1-m increase in elevation; 2) the grassland NPP was positively correlated with temperature in alpine meadow (AM, 2,700–3,500 m asl), mid-mountain forest meadow (MMFM, 1,650–2,700 m asl) and low-mountain dry grassland (LMDG, 650–1,650 m asl), while positive correlations were found between NPP and annual precipitation in plain desert grassland (PDG, lower than 650 m asl); 3) an increase (from 0.08 to 1.09 g C/(m2×a)) in mean NPP for the grassland in TMJB under a real climate change scenario was observed from 1959 to 2009; and 4) remarkable differences in WUE were found among different elevations. In general, WUE increased with decreasing elevation, because water availability is lower at lower elevations; however, at elevations lower than 540 m asl, we did observe a decreasing trend of WUE with decreasing elevation, which may be due to the sharp changes in canopy cover over this gradient. Our research suggests that the NPP simulated by Biome-BGC is consistent with field data, and the modeling provides an opportunity to further evaluate interactions between environmental factors and ecosystem productivity.
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QiFei HAN
GePing LUO
ChaoFan LI
Hui YE
YaoLiang CHEN
关键词:  water and salt transportation  furrow irrigation  saline water  soil salinity  soil water content    
Abstract: Mountainous ecosystems are considered highly sensitive and vulnerable to natural disasters and climatic changes. Therefore, quantifying the effects of elevation on grassland productivity to understand ecosystem-climate interactions is vital for mountainous ecosystems. Water-use efficiency (WUE) provides a useful index for understanding the metabolism of terrestrial ecosystems as well as for evaluating the degradation of grasslands. This paper explored net primary productivity (NPP) and WUE in grasslands along an elevational gradient ranging from 400 to 3,400 m asl in the northern Tianshan Mountains–southern Junggar Basin (TMJB), Xinjiang of China, using the Biome-BGC model. The results showed that: 1) the NPP increased by 0.05 g C/(m2×a) with every increase of 1-m elevation, reached the maximum at the mid-high elevation (1,600 m asl), and then decreased by 0.06 g C/(m2×a) per 1-m increase in elevation; 2) the grassland NPP was positively correlated with temperature in alpine meadow (AM, 2,700–3,500 m asl), mid-mountain forest meadow (MMFM, 1,650–2,700 m asl) and low-mountain dry grassland (LMDG, 650–1,650 m asl), while positive correlations were found between NPP and annual precipitation in plain desert grassland (PDG, lower than 650 m asl); 3) an increase (from 0.08 to 1.09 g C/(m2×a)) in mean NPP for the grassland in TMJB under a real climate change scenario was observed from 1959 to 2009; and 4) remarkable differences in WUE were found among different elevations. In general, WUE increased with decreasing elevation, because water availability is lower at lower elevations; however, at elevations lower than 540 m asl, we did observe a decreasing trend of WUE with decreasing elevation, which may be due to the sharp changes in canopy cover over this gradient. Our research suggests that the NPP simulated by Biome-BGC is consistent with field data, and the modeling provides an opportunity to further evaluate interactions between environmental factors and ecosystem productivity.
Key words:  water and salt transportation    furrow irrigation    saline water    soil salinity    soil water content
收稿日期:  2013-02-05      修回日期:  2013-04-20           出版日期:  2013-09-10      发布日期:  2013-09-10      期的出版日期:  2013-09-10
基金资助: 

This research is funded by the National Natural Science Foun-dation of China (41271126) and the National Basic Research Program of China (2009CB825105).

通讯作者:  GePing LUO    E-mail:  luogp@ms.xjb.ac.cn
引用本文:    
QiFei HAN, GePing LUO, ChaoFan LI, Hui YE, YaoLiang CHEN. Modeling grassland net primary productivity and water-use efficiency along an elevational gradient of the Northern Tianshan Mountains[J]. 干旱区科学, 2013, 5(3): 354-365.
QiFei HAN, GePing LUO, ChaoFan LI, Hui YE, YaoLiang CHEN. Modeling grassland net primary productivity and water-use efficiency along an elevational gradient of the Northern Tianshan Mountains. Journal of Arid Land, 2013, 5(3): 354-365.
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http://jal.xjegi.com/CN/10.1007/s40333-013-0182-y  或          http://jal.xjegi.com/CN/Y2013/V5/I3/354
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