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Featured researches published by Liu Jing-shuang.


Chinese Geographical Science | 2002

SPATIAL-TEMPORAL VARIATION OF HEAVY METAL ELEMENTS CONTENT IN COVERING SOIL OF RECLAMATION AREA IN FUSHUN COAL MINE

Yu Jun-bao; Liu Jing-shuang; Wang Jin-da; Li Zhong-gen; Zhang Xue-lin

Grid method is employed for sampling covering soil at the test field, which is reclamation area filled by coal mining wastes for cropland in the Fushun coal mine, Liaoning Province, the Northeast China. The soil samples are taken at different locations, including three kinds of covering soil, three different depths of soil layers and four different covering ages of covering soil. The spatial-temporal variation of heavy metal element content in reclamation soil is studied. The results indicate that the content of heavy metal elements is decreasing year after year; the determinant reason why the content of heavy metal elements at 60cm depth layer is higher than that at 30cm depth layer and surface is fertilizer and manure application; the metal elements mainly come from external environment; there is no metal pollution coming from mother material (coal mining wastes) in plough layer of covering soil.


Acta Ecologica Sinica | 2007

Biogeochemical cycle of Sulfer in the Calamagrostis angustifolia wetland ecosystem in the Sanjiang Plain, China

Li Xinhua; Liu Jing-shuang; Wang Jin-da; Sun Zhigao; Yang Jisong

Abstract To better understand the Sulfur (S) cycle in the wetland ecosystem, the S cycle and its compartmental distribution within an atmosphere-plant-soil system were studied using a compartment model in the Calamagrostis angustifolia wetland in the Sanjiang Plain, Northeast China. The results showed that the soil was the main S storage and flux hinge in which 97.78% S was accumulated. In the plant subsystem, the root was the main S storage, and it remained at 79.60% of the total S contents, which in the Calamagrostis angustifolia wetland ecosystem showed that the parts above the ground took up 0.75 g S/m2, the S re-transferring biomass to the root was 0.24 g S/m2, and to the litter was 0.51 g S/m2; the root took up 3.76 g S/m2 and the S transferring biomass to the soil took up 3.07 g S/m2; the litter S biomass was 0.75 g S/(m2·a) and the S transferring biomass to the soil was more than 0.52 g S/(m2·a). The emission amount of H2S from the Calamagrostis angustifolia wetland ecosystem to the atmosphere was 1.42 mg S/m2, whereas carbonyl sulfide (COS) was absorbed by the Calamagrostis angustifolia wetland from the atmosphere and the absorption amount was 1.83 mg S/m2. The S input biomass from the rain to the ecosystem was 4.85mg S/m2 during the growing season. The difference between input and output amounts was 5.26 mg S/m2, which indicated that S was accumulated in the ecosystem and would lead to wetland acidification in the future.


Chinese Geographical Science | 1999

Dynamic variation of nitrogen content in the Second Songhua River

Liu Jing-shuang; Yu Jun-bao

The space-time variation laws of nitrogen content in different river sections, water periods and years in the Second Songhua River in China is described in detail. The results show that there is direct relation between the nitrogen content variation in river water and that in wastewater from cities and runoff water of both banks of the river. Nitrate and nitrite contents in water in flood period are higher than that in mid and low water periods. In flood period, nitrate content in water increases gradually with the extension of river section, ammonia content in polluted river section is higher than that in unpolluted river section. Nitrate and nitrite contents in water in the flood, mid and low water periods from 1985 to 1989 were slightly higher than that from 1980 to 1984 and from 1990 to 1994, ammonia content in water increased annually.


Human and Ecological Risk Assessment | 2016

Source identification and availability of heavy metals in peri-urban vegetable soils: A case study from China

Liu Qiang; Liu Jing-shuang; Wang Qicun; Wang Yang

ABSTRACT The purpose of this study was to investigate the total and available concentrations of Pb, Cr, Cu, Ni, and Zn in the vegetable soils from the outskirts of a heavy industry city, Northeast China, and to assess the sources of heavy metals and their availability. The average concentrations of Pb, Cu, and Zn were significantly higher than their background values of Changchun topsoil. Principal component analysis, cluster analysis, and geostatistical analysis results suggested that Pb, Cu, and Zn were consistently from anthropogenic sources, while Cr and Ni were from natural sources with low concentrations. Kriging results showed that several hotspots of high metal concentration were identified by the geochemical maps and caused by different environmental factors. Although the available (ethylene-diamine-tetraacetic acid-extractable) fractions showed much lower values than total concentrations of metals, Pb and Cu had relatively high ARa (average availability ratio of metals) values. Our findings show that most of the studied metals had accumulated to some extent in vegetable soils and several hotspots of high metal concentration appeared at the peri-urban of Changchun. The concentrations of some metals in peri-urban vegetable soils have been largely affected by anthropogenic activities. Appropriate measures should be taken to effectively control heavy metal levels in vegetable soils and thus protect human health.


Frontiers of Forestry in China | 2007

Biomass structure and nitrogen, phosphorus nutrient of Calamagrostis angustifolia populations in different communities of Sanjiang Plain, Northeast China

Sun Zhigao; Qin Shengjin; Liu Jing-shuang; Wang Jin-da

Calamagrostis angustifolia is the dominant species in the typical meadow and marsh meadow communities of Sanjiang Plain. The study on its biomass, the nitrogen (N) and phosphorus (P) contents in its different organs showed that the biomass of different C. angustifolia organs in the two types of wetland communities was distinctly different, which could be described by polynomial. The biomass of aboveground part and each organ presented single peak changing, with the maximum value of the latter occurred 15 days after. The F/C values were all less than 1, which were bigger in typical meadow than those in marsh meadow. The total N and P contents in different organs of aboveground part all descended monotonically in growth season, with the order of leaf>vagina>stem. The change of total N content in roots of the two types of C. angustifolia was consistent, while that of total P was quite different. The content of total N, ammonium nitrogen (NH4+-N) and nitrate nitrogen (NO3−-N), especially of NH4+-N and NO3−-N, varied widely in different organs, with NH4+-N/NO3−-N>1. Root was the important storage of N and P, but the storage of N and P in stem, leaf and vagina fluctuated greatly. The N/P ratios of the two types of C. angustifolia were all less than 14, which implied that N might be the limiting nutrient of C. angustifolia, and the limitation degree was higher in typical meadow than that in marsh meadow.


Environmental Geochemistry and Health | 2015

Grain-size distribution and heavy metal contamination of road dusts in urban parks and squares in Changchun, China.

Liu Qiang; Wang Yang; Liu Jing-shuang; Wang Quanying; Zou Mingying


Chinese Geographical Science | 2006

DISTRIBUTION OF LEAD IN URBAN SOIL AND ITS POTENTIAL RISK IN SHENYANG CITY, CHINA

Wang Jin-da; Ren Hui-Min; Liu Jing-shuang; Yu Jun-bao; Zhang Xue-lin


Progress in geography | 2011

An Application Study of DEM Based Distributed Hydrological Model on Macroscale Watershed

Sun Zhigao; Liu Jing-shuang; Yu Junbao; Wang Jin-da


Journal of Arid Land Resources and Environment | 2006

The Actuality,Problems and Sustainable Utilization Countermeasures of Wetland Resources in China

Sun Zhigao; Liu Jing-shuang; Li Bin


Chinese Journal of Soil Science | 2006

Mechanism of Phosphorus Availability Changing in Soil

Qin Shengjin; Liu Jing-shuang

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Wang Yang

Chinese Academy of Sciences

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Wang Jin-da

Chinese Academy of Sciences

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Sun Zhigao

Chinese Academy of Sciences

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Zhao GuangYing

Chinese Academy of Sciences

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Yang Jisong

Chinese Academy of Sciences

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Yu Jun-bao

Chinese Academy of Sciences

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Dou Jing-xin

Chinese Academy of Sciences

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Liu Qiang

Chinese Academy of Sciences

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Qin Shengjin

Chinese Academy of Sciences

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Li Xinhua

Chinese Academy of Sciences

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