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Featured researches published by Li Shuangcheng.


Journal of Geographical Sciences | 2006

Characteristics of grassland degradation and driving forces in the source region of the Yellow River from 1985 to 2000

Liu Linshan; Zhang Yili; Bai Wanqi; Yan Jianzhong; Ding Mingjun; Shen Zhenxi; Li Shuangcheng; Zheng Du

The source region of the Yellow River is located in the middle east of the Tibetan Plateau in northwest China. The total area is about 51,700 km2, mainly covered by grassland (79%), unused land (16%) and water (4%). The increasing land utilization in this area has increased the risk of environmental degradation. The land use/cover data (1985 and 2000) provided by the Data Center of Resources and Environment in the Chinese Academy of Sciences were used to analyze the land cover change in the source region of the Yellow River. DEM (1:250,000) data, roads and settlement data were used to analyze the spatial characteristics of grasslands degradation. The ArcGIS 9 software was used to convert data types and do the overlay, reclassification and zonal statistic analysis. Results show that grassland degradation is the most important land cover change in the study area, which occupied 8.24% of the region’s total area. Human activities are the main causes of the grassland degradation in the source region of the Yellow River: 1) the degradation rate is higher on the sunny slope than on the shady slope; 2) the grassland degradation rate decreases with an increase in the elevation, and it has a correlation coefficient of −0.93; 3) the nearer to the settlements the grassland is, the higher the degradation rate. Especially within a distance range of 12 km to the settlements, the grassland degradation rate is highly related with the distance, with a coefficient of −0.99; and 4) in the range of 4 km, the degradation rate decreases with the increase of distance to the roads, with a correlation coefficient of −0.98. Besides some physical factors, human activities have been the most important driving forces of the grassland degradation in the source region of the Yellow River since 1985. To resolve the degradation problems, population control is essential, and therefore, it can reduce the social demand of livestock products from the grassland. To achieve sustainable development, it needs to improve the management of grassland ecosystem.


Chinese Science Bulletin | 2007

Ecosystem vulnerability of China under B2 climate scenario in the 21st century

Wu Shaohong; Dai Erfu; Huang Mei; Shao Xuemei; Li Shuangcheng; Tao Bo

This paper applies climate change scenarios in China based on the SRES assumptions with the help of RCMs projections by PRECIS (providing regional climates for impacts studies) system introduced to China from the Hadley Centre for Climate Prediction and Research at a high-resolution (50 km×50 km) over China. This research focuses on B2 scenario of SRES. A biogeochemical model “Atmosphere Vegetation Integrated Model (AVIM2)” was applied to simulating ecosystem status in the 21st century. Then vulnerability of ecosystems was assessed based on a set of index of mainly net primary production (NPP) of vegetation. Results show that climate change would affect ecosystem of China severely and there would be a worse trend with the lapse of time. The regions where having vulnerable ecological background would have heavier impacts while some regions with better ecological background would also receive serious impacts. Extreme climate even would bring about worse impact on the ecosystems. Open shrub and desert steppe would be the two most affected types. When the extreme events happen, vulnerable ecosystem would extend to part of defoliate broad-leaved forest, woody grassland and evergreen conifer forest. Climate change would not always be negative. It could be of some benefit to cold region during the near-term. However, in view of mid-term to long-term negative impact on ecosystem vulnerability would be enormously.


Chinese Geographical Science | 2003

Impact of road construction on vegetation alongside Qinghai-Xizang highway and railway

Chen Hui; Li Shuangcheng; Zhang Yili

Based on the field investigation in August 2001 and August 2002, digital China Vegetation Map in 2001 and Qinghai-Xizang (Tibet) Plateau Vegetation Regionalization Map in 1996, vegetation characteristics along two sides of Qinghai-Xizang highway and railway are studied in this paper. Meanwhile, the impact of Qinghai-Xizang highway and railway constructions on the vegetation types are analyzed using ARCVIEW, ARC/INFO and PATCH ANALYSIS. It was found that: 1) Qinghai-Xizang highway and railway span 9 latitudes, 12 longitudes and 6 physical geographic regions (East Qinghai and Qilian mountain steppe region, Qaidam mountain desert region, South Qinghai-Xizang alpine meadow steppe region, Qiangtang alpine steppe region, Golog-Nagqu alpine shrub meadow region and South Xizang mountain shrub steppe region); 2) the construction of Qinghai-Xizang highway and railway destroyed natural vegetation and landscape, especially in 50m-wide buffer regions along both sides of the roads, it was estimated that the net primary productivity deceased by about 30 504.62t/a and the gross biomass deceased by 432 919.25–1 436 104.3t. The losing primary productivity accounted for 5.70% of the annual primary productivity within 1km-wide buffer regions (535 005.07–535 740.11t/a), and only 0.80%–0.89% of that within 10km-wide buffer regions (3 408 950.45–3 810 480.92t/a). The losing gross biomass was about 9.47%–17.06% of the gross biomass within 1km-wide buffer regions (7 502 971.85–25 488 342.71t), and only 1.47%–2.94% of that within 10km-wide buffer regions (43 615 065.35–164 150 665.37t).


Journal of Geographical Sciences | 2006

Surface pollen in the east of Qaidam Basin

Chen Hui; Zhao Dongsheng; Lu Xinmiao; Li Yuecong; Xu Qinghai; Li Shuangcheng; Ouyang Hua

Pollen analysis of 23 surface samples in the east of Qaidam Basin reveals the characteristics of pollen assemblages and their relationships with vegetation and climate. In pollen assemblages, Chenopodiaceae and Artemisia are preponderant types in all the samples, and Ephedra, Gramineae and Compositae are common types. The results of DCA (Detrended Correspondance Analysis) and Correlation Analysis show different pollen assemblages indicate different vegetations, coincided with respective vegetation types. A/C (Artemisia/Chenopodiaceae) in the desert can indicate the aridity. Depending on the aridity, the vegetation communities are divided into four groups: severe drought group, moderate drought group, slight drought group and tropophilous group. A/C value is less 0.2 in the severe drought group, 0.2–0.5 in the moderate drought group, 1.63 in the slight drought group and 5.72 slight-wetness group.


Human and Ecological Risk Assessment | 2007

Ecological risk assessment of regions along the roadside of the Qinghai-Tibet highway and railway based on an artificial neural network

Chen Hui; Liu Jinsong; Cao Yu; Li Shuangcheng; Ouyang Hua

ABSTRACT A concept model of regional risk was constructed for the characteristics of ecosystems alongside the Qinghai-Tibet highway and railway based on the MLP (Multilayer perceptron) model. Seven indices such as snow hazard, drought hazard, and landslide were selected in order to evaluate the integrated ecological risk of the ecosystems along the study area. Results show that the Qaidam montane desert zone had the greatest average risk value (4.26), followed by the Golog-Nagqu high-cold scrub meadow zone (2.80) and the East Qinghai and Qilian montane steppe zone (2.73) among the ecosystems within the six natural zones within the study region. As far as land cover types are concerned, the top three ecological risk values appear in the needle-leaved forest (4.31), desert (4.12), and land without vegetation (3.62), which are higher than those in the other seven types in the study site. Although the risk values are influenced by natural factors and human activities, they are more strongly controlled by natural factors. According to the ecological risk characteristics, the ecosystems within the study area are subdivided into four subregions, including the Qaidam basin region (high risk), the Xidatan to Damxung region (moderate risk), and the Eastern Qinghai-Qilian (slight risk) and Southern Xizang (Tibet) region (slighter risk).


Chinese journal of population, resources and environment | 2012

Impact of Climate Change on Urban Agglomerations in China’s Coastal Region

Dong Suocheng; Tao Shu; Yang Wangzhou; Li Fei; Li Shuangcheng; Li Yu; Liu Hongyan

Abstract Climate change and urbanization issues are the two key factors that make humans liable to be affected by disasters, which are overlapped in urban agglomeration. The five big urban agglomerations of China with strong economic power are the important engines for national economic and social development. However, being in the sea-land mutual interaction belts with a vast hazard-bearing body, they are affected by sea-land compound disasters, and are liable to suffer heavy disaster losses with climate change. It is suggested that government departments concerned should fully recognize the impact of climate change on coastal urban agglomerations, propose strategies as soon as possible, and integrate the impact of climate change and adaptation countermeasures into the various kinds of social-economic development plans for coastal urban regions.


International Journal of Climatology | 2006

MEASUREMENT OF CLIMATE COMPLEXITY USING SAMPLE ENTROPY

Li Shuangcheng; Zhou Qiaofu; Wu Shaohong; Dai Erfu


Ecological Indicators | 2009

Indicating landscape fragmentation using L–Z complexity

Li Shuangcheng; Chang Qing; Peng Jian; Wang Yanglin


Beijing Daxue Xuebao. Zirankexueban | 2009

GISと土壌浸食方程式に基づく農業生態系土壌保全価値評価-以京津冀地域を例として-【JST・京大機械翻訳】

Gao Jiangbo; Zhou Qiaofu; Chang Qing; Li Shuangcheng


Beijing Daxue Xuebao. Zirankexueban | 2009

省エネルギーに基づく生態学的フットプリントモデルの改良に基づき,1978~2006年の生態学的経済システムの分析を行った。【JST・京大機械翻訳】

Zhao Zhiqiang; Gao Jiangbo; Li Shuangcheng; Wang Yanglin

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Chen Hui

Hebei Normal University

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Dai Erfu

Chinese Academy of Sciences

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Wu Shaohong

Chinese Academy of Sciences

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Zhang Yili

Chinese Academy of Sciences

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Cao Yu

Zhejiang University

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Chang Qing

China Agricultural University

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Ding Mingjun

Jiangxi Normal University

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Dong Suocheng

Chinese Academy of Sciences

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Huang Mei

Chinese Academy of Sciences

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Li Fei

Chinese Academy of Sciences

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