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mass-balance ecosystem model of the East China Sea

Progress in Natural Science:Materials International 2009年第10期19卷 1271-1280页

作者： William W.L. Cheung Tony J. Pitcher The Fisheries Centre University of British Columbia

Using the Ecopath mass-balance trophodynamic model,this paper analyzed the trophic levels,flows,food web structure and ecosystem maturity of the East China Sea,and identified ecologically important functional groups in the *** model is based on fishery resource surveys of the East China Sea in 2000,studies on diet composition and global databases such as FishBase and the Sea Around Us Project *** results showed that trophic levels of the functional groups are between 2.86 and 4.37,with an average of ***(Engraulis japonicus),small fishes and benthic crustaceans such as shrimps and crabs are important groups in terms of the trophic structure and flow dynamics in the East China *** flows of most groups are between specific trophic levels,except file fish(Thamnaconus spp.),pomfret(Pampus spp.) and *** transfer efficiency of levels Ⅱ,Ⅲ,IV and more than V are 11.8%,21.1%,17.4% and 22.1-22.5%,*** of fishery-the largest ‘consumer’ of the ecosystemare much stronger than those exerted by biological groups in the *** model suggests that the current fishery can further reduce the complexity of the *** of the system indices suggest that maturity of the ecosystem is *** conclusion of this model indicates that it was the overfishing that caused the ecosystem of the East China Sea declined,which should be taken into account as a critical reference for fisheries management in the future.

关键词： Ecopath East China Sea mass-balance Fishery Ecosystem

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The mass-balance characteristics and sensitivities to climate variables of Laohugou Glacier No.12,western Qilian Mountains,China

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Research in Cold and Arid Regions 2017年第6期9卷 631-641页

作者： JiZu Chen ShiChang Kang Xiang Qin WenTao Du WeiJun Sun YuShuo Liu Qilian Shan Station of Glaciology and Ecological Environment State Key Laboratory of Cryospheric SciencesNorthwest Institute of Eco-Environment and ResourcesChinese Academy of SciencesLanzhouGansu 730000China University of CAS Beijing 100049China CAS Center for Excellence in Tibetan Plateau Earth Sciences Beijing 100085China College of Population Resources and EnvironmentShandong Normal UniversityJinanShandong 250014China

Due to global warming, glaciers on the Tibetan Plateau(TP) are experiencing widespread shrinkage; however, the mechanisms controlling glacier variations across the TP are still rather unclear, especially on the northeastern TP. In this study, a physically based, distributed surface-energy and mass-balance model was used to simulate glacier mass balance forced by meteorological data. The model was applied to Laohugou No. 12 Glacier, western Qilian Mountains, China, during2010~2012. The simulated albedo and mass balance were validated and calibrated by in situ measurements. The simulated annual glacier-wide mass balances were-385 mm water equivalent(w.e.) in 2010/2011 and-232 mm w.e. in 2011/2012,respectively. The mean equilibrium-line altitude(ELA) was 5,015 m a.s.l., during 2010~2012, which ascended by 215 m compared to that in the 1970 s. The mean accumulation area ratio(AAR) was 39% during the two years. Climatic-sensitivity experiments indicated that the change of glacier mass balance resulting from a 1.5 °C increase in air temperature could be offset by a 30% increase in annual precipitation. The glacier mass balance varied linearly with precipitation, at a rate of130 mm w.e. per 10% change in total precipitation.

关键词： glacier mass balance energy- and mass-balance model climate sensitivities

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Glacier mass-balance Variation in China during the Past Half Century

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Journal of Geoscience and Environment Protection 2018年第5期6卷 37-58页

作者： Yousif Elnour Yagoub Zhongqin Li Ahmed A. H. Siddig Omer Said Musa Muhammad Naveed Anjum State Key Laboratory of Cryospheric Sciences/Tian Shan Glaciological Station Northwest Institute of Eco-Environment and Resources CAS Lanzhou China Faculty of Forestry Department of Forest Protection and Conservation University of Khartoum Shambat Sudan Division of Hydrology Water-Land Resources Northwest Institute of Eco-Environment and Resources CAS Lanzhou China

The aim of this study is to investigate the impact of temperature trend on glacier-mass balance, snow density, snowmelt, snow depth and runoff by using observations of nine glacier stations that covered most of the China over the period of 1979-2013. Trend analysis showed an increasing trend of temperature on all of the selected stations. On an average, temperature was increasing at the rate of 0.46/10a. The increasing trend of temperature showed a negative relationship with annual glacier-mass balance on most of the stations and caused a decrease in annual balance. Results of Pearson’s correlation analysis showed a highly significant negative correlation between temperature and snow density (correlation coefficient (CC = -0.661 at 0.01 significance level). There was a significant positive correlation between temperature and snowmelt (CC = 0.532 at 0.01 significance level). There was a significant negative correlation between temperature and snow depth (correlation coefficient (CC = -0.342 at 0.05 significance level). Moreover, there was a significant positive correlation between temperature and runoff (CC = 0.586 at 0.01 significance level). Increasing trend of temperature caused an increasing trend of annual snowmelt and runoff anomaly% at the rate of 24.82/10a and 9.87/10a, respectively. On the other hand, a declining trend in annual snow density and snow depth anomaly% was found at a rate of -5.32/10a and -1.93/10a, respectively. We concluded that the snow density, snowmelt and runoff are significantly sensitive to temperature in China. This contribution has provided information for further understanding of glacier variation and its influencing factors.

关键词： Glacier mass-balance Snow Density Snowmelt Snow Depth Runoff Climate Variation

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Uncertainties in the Mercury mass balance in a Coal-Based IGCC Power Plant (Puertollano, Spain)

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Energy Engineering 2021年第4期118卷 1223-1235页

作者： José María Esbrí Alba Martinez-Coronado Sofía Rivera Jurado Eva García-Noguero Pablo Higueras Instituto de Geología Aplicada(UCLM) Pl.Manuel Meca1Ciudad Real13400Spain

Mercury(Hg)is a global pollutant that is subject to strict regulations to reduce anthropogenic *** production of energy represents an important activity that leads to Hg emissions into the *** all the systems used,IGCC plants are the most promising for reducing Hg emissions,since it is possible to remove Hg from syngas prior to *** aim of the present work was to evaluate the presence of Hg in the main streams of an experimental IGCC plant(ELCOGAS,Puertollano)in order to quantify Hg emissions and investigate the possibility of reducing *** main streams of the system were sampled for three consecutive days and both the solids,i.e.,raw material(coal and petroleum coke),fine and coarse slags,fly ash,sulphur,and the liquids,i.e.,slag system,Venturi scrubber and saturator,were *** results show that an average of 12.9%of the Hg that enters the IGCC power plant is eliminated with solid waste and only 0.08%with liquid *** is still an average of 87.12%of Hg that is not accounted for in the mass balance and that could remain in the system and/or be eliminated in the streams that were not *** it is impossible to offer an explanation for the final fate of the Hg lost in the system based on the obtained results,the data suggest that sulphur byproducts could be primarily responsible for the elimination of Hg from the syngas,and that a major proportion of Hg should be emitted via the chimney after the syngas combustion process.

关键词： Mercury IGCC power plant mass-balance hypercinnabar

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