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陆地生态系统碳氮水循环的关键耦合过程及其生物调控机制探讨 被引量:72
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作者 于贵瑞 高扬 +2 位作者 王秋凤 刘世荣 申卫军 《中国生态农业学报》 CAS CSCD 北大核心 2013年第1期1-13,共13页
陆地生态系统碳循环、氮循环和水循环是全球变化科学研究的三大主题,而陆地生态系统碳氮水耦合循环过程及其生物调控机制则是全球变化生态学研究的前沿性科学问题。目前,对陆地生态系统碳氮水耦合循环过程及其调控机制认识的不足是制约... 陆地生态系统碳循环、氮循环和水循环是全球变化科学研究的三大主题,而陆地生态系统碳氮水耦合循环过程及其生物调控机制则是全球变化生态学研究的前沿性科学问题。目前,对陆地生态系统碳氮水耦合循环过程及其调控机制认识的不足是制约评估陆地增汇/减排效果,预测分析全球变化对生态系统生产力和固碳功能影响的瓶颈性问题。本文在综合分析陆地生态系统碳氮水循环的耦合过程基础上,论述了制约生态系统碳氮水循环空间格局耦联关系的生物地理学机制,制约典型生态系统碳氮水循环耦合关系的生物生理生态学机制,以及典型生态系统碳氮水耦合循环的关键生物物理和生物化学过程。重点评述了生态系统碳氮水耦合循环的主要过程及其生物调控机制研究进展,包括:(1)植物叶片冠层生物学过程和根系冠层生物学过程及其对生态系统碳氮水耦合循环控制机制,以及二者之间的关联与互作关系;(2)土壤微生物功能群网络及其对碳氮循环过程的影响;(3)生态系统碳氮水交换通量的时空变化规律,以及生态系统的生态化学计量学理论与实践。本文最后还简要介绍了国家基金委重大研究项目"森林生态系统碳氮水耦合循环的生物控制机制"的研究思路及其主要研究内容。期望能够通过这些探讨对推动我国该研究领域的基础理论建设和新技术发展有所贡献。 展开更多
关键词 陆地生态系统 --耦合循环 生物调控机制 叶片冠层 根系冠层 土壤微生物功能群网络
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陆地生态系统水—碳耦合循环与过程管理研究 被引量:55
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作者 于贵瑞 王秋凤 于振良 《地球科学进展》 CAS CSCD 2004年第5期831-839,共9页
陆地生态系统的水循环与碳循环是地球表层系统物质循环与能量交换的核心,也是最基本的耦合的两个生态学过程。区域或全球尺度生态系统的水管理与碳管理是全球变化科学与可持续发展研究的两大主题,是人类维持全球生态系统的物质与能量循... 陆地生态系统的水循环与碳循环是地球表层系统物质循环与能量交换的核心,也是最基本的耦合的两个生态学过程。区域或全球尺度生态系统的水管理与碳管理是全球变化科学与可持续发展研究的两大主题,是人类维持全球生态系统的物质与能量循环、自然资源循环再生的重要生态学途径。我们在综合评述现代应用生态学研究的发展趋势,陆地生态系统水和碳循环与生态系统管理关系的基础上,提出了陆地生态系统水循环与碳循环过程管理的内容与思路,阐述了生态系统水和碳耦合循环机制与模拟综合研究的新设想。 展开更多
关键词 陆地生态系统 生态系统-耦合循环 生态系统管理 生态系统管理 生态系统管理
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陆地生态系统碳-氮-水耦合循环的基本科学问题、理论框架与研究方法 被引量:23
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作者 于贵瑞 王秋凤 方华军 《第四纪研究》 CAS CSCD 北大核心 2014年第4期683-698,682,共16页
陆地生态系统碳循环、氮循环和水循环是生态系统生态学和全球变化科学研究长期被关注的三大物质循环,它们表征着全球、区域及典型生态系统的能量流动、养分循环和水循环。然而,自然界的生态系统碳循环、氮循环和水循环是相互联动、不可... 陆地生态系统碳循环、氮循环和水循环是生态系统生态学和全球变化科学研究长期被关注的三大物质循环,它们表征着全球、区域及典型生态系统的能量流动、养分循环和水循环。然而,自然界的生态系统碳循环、氮循环和水循环是相互联动、不可分割的耦合体系,在生态学、生理学、生物化学等方面受多个生物、物理、化学和生物学过程的调节和控制。本文在综合论述陆地生态系统碳-氮-水耦合循环研究的理论和实践意义的基础上,探讨了陆地生态系统碳-氮-水耦合循环的关键过程,提出该研究领域的基本科学问题,重点分析了植被-大气、土壤-大气和根系-土壤3个界面上碳、氮、水交换的生物物理过程,典型生态系统碳-氮-水耦合循环的生物学化学过程,制约典型生态系统碳-氮-水循环耦合关系的生态系统生态学机制,以及制约生态系统碳-氮-水循环空间格局耦联关系的生物地理生态学机制。在现有科学研究的基础上,构建了陆地生态系统碳-氮-水耦合循环机制的逻辑框架系统,讨论了开展陆地生态系统碳-氮-水耦合循环研究的主要技术途径与方法。 展开更多
关键词 陆地生态系统--耦合循环 耦合循环的关键过程 耦合关系的形成机制 生态系统生态学机制 生物地理生态学机制
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The integration of nitrogen dynamics into a land surface model. Part 1: model description and site-scale validation 被引量:2
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作者 YANG Xiujing DAN Li +5 位作者 YANG Fuqiang PENG Jing LI Yueyue GAO Dongdong JI Jinjun HUANG Mei 《Atmospheric and Oceanic Science Letters》 CSCD 2019年第1期50-57,共8页
Nitrogen cycling has profound effects on carbon uptake in the terrestrial ecosystem and the response of the biosphere to climate changes.However,nutrient cycling is not taken into account in most land surface models f... Nitrogen cycling has profound effects on carbon uptake in the terrestrial ecosystem and the response of the biosphere to climate changes.However,nutrient cycling is not taken into account in most land surface models for climate change.In this study,a nitrogen model,based on nitrogen transformation processes and nitrogen fluxes exchange between the atmosphere and terrestrial ecosystem,was incorporated into the Atmosphere–Vegetation Interaction Model(AVIM)to simulate the carbon cycle under nitrogen limitation.This new model,AVIM-CN,was evaluated against site-scale eddy covariance–based measurements of an alpine meadow located at Damxung station from the FLUXNET 2015 dataset.Results showed that the annual mean gross primary production simulated by AVIM-CN(0.7073 gC m^-2 d^-1)was in better agreement with the corresponding flux data(0.5407 gC m^-2 d^-1)than the original AVIM(1.1403 gC m^-2 d^-1)at Damxung station.Similarly,ecosystem respiration was also down-regulated,from 1.7695 gC m^-2 d^-1 to 1.0572 gC m^-2 d^-1,after the nitrogen processes were introduced,and the latter was closer to the observed vales(0.8034 gC m^-2 d^-1).Overall,the new results were more consistent with the daily time series of carbon and energy fluxes of observations compared to the former version without nitrogen dynamics.A model that does not incorporate the limitation effects of nitrogen nutrient availability will probably overestimate carbon fluxes by about 40%. 展开更多
关键词 Coupled carbon and nitrogen dynamics nitrogen limitation land surface model carbon–nitrogen–water cycles
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万华岩表层岩溶带岩溶动力系统的特点研究 被引量:6
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作者 姜光辉 郭芳 +3 位作者 张美良 何师意 李恩香 邓艳 《中国岩溶》 CAS CSCD 2002年第3期173-177,187,共6页
万华岩地区碳酸盐岩中普遍发育的非碳酸盐岩夹层 ,以及“土层 +裂隙层”表层岩溶带双层结构对岩溶动力系统和水循环具有显著影响 :非碳酸盐岩地段的地下水因其矿化度较低 ,CO2 含量较高 ,而具有较强的侵蚀、溶蚀能力 ,导致岩溶动力系统... 万华岩地区碳酸盐岩中普遍发育的非碳酸盐岩夹层 ,以及“土层 +裂隙层”表层岩溶带双层结构对岩溶动力系统和水循环具有显著影响 :非碳酸盐岩地段的地下水因其矿化度较低 ,CO2 含量较高 ,而具有较强的侵蚀、溶蚀能力 ,导致岩溶动力系统的物质和能量传输非常活跃 ,一个岩溶泉年溶蚀量 (以 Ca CO3计 )达2 795 .4 kg;由于非碳酸盐岩夹层的普遍存在 ,不仅阻碍地下水向深循环 ,而且还有利于土壤、植被的发育。土壤、植被与地表岩溶裂隙网络对区内岩溶地下水还具有较好的调蓄作用 ,以致使区内有众多的小泉点在地表出露。 展开更多
关键词 岩溶动力系统 表层岩溶带 酸盐岩夹层 碳-水循环 地下 矿化度 溶蚀能力
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Synthesis and application of an environmentally friendly antiscalant in industrial cooling systems
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作者 黄镜怡 刘广卿 +2 位作者 薛蒙伟 周钰明 姚清照 《Journal of Southeast University(English Edition)》 EI CAS 2014年第4期514-519,共6页
Allylpolyethoxy carboxylate macromonomers possessing polyethylene oxygen long chains were synthesized by advanced technology of the polyether cap.A novel double-hydrophilic block copolymer was prepared through free ra... Allylpolyethoxy carboxylate macromonomers possessing polyethylene oxygen long chains were synthesized by advanced technology of the polyether cap.A novel double-hydrophilic block copolymer was prepared through free radical polymeric reactions in aqueous solution and its performance on CaCO3 inhibition and dispersancy activity towards Fe2 O3 was evaluated in recirculating cooling water systems.The study shows that acrylic acid-allylpolyethoxy carboxylate has a significant ability to inhibit the precipitation of calcium carbonate and an excellent dispersing capability to stabilize iron Ⅲ in industrial cooling systems. X-ray diffraction shows that there is a number of vaterite crystals in the presence of the phosphorous free and non-nitrogen copolymer. The change in crystal forms is also confirmed by the Fourier-transform infrared spectra the scanning electron microscopy and the transmission electron microscopy. The inhibition mechanism is proposed and it shows that the interactions between calcium and polyethylene glycol PEG are the fundamental impetus for restraining the formation of the scale in cooling water systems. 展开更多
关键词 phosphorous free antiscalant calcium carbonate industrial cooling systems phosphorous free antiscalant calcium carbonate industrial cooling systems
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Influence of Climate on Soil Organic Carbon in Chinese Paddy Soils 被引量:2
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作者 WANG Dandan YAN Yechao +5 位作者 LI Xinhui SHI Xuezheng ZHANG Zhongqi David C WEINDORF WANG Hongjie XU Shengxiang 《Chinese Geographical Science》 SCIE CSCD 2017年第3期351-361,共11页
Soil organic carbon(SOC) is a major component of the global carbon cycle and has a potentially large impact on the greenhouse effect. Paddy soils are important agricultural soils worldwide, especially in Asia. Thus, a... Soil organic carbon(SOC) is a major component of the global carbon cycle and has a potentially large impact on the greenhouse effect. Paddy soils are important agricultural soils worldwide, especially in Asia. Thus, a better understanding of the relationship between SOC of paddy soils and climate variables is crucial to a robust understanding of the potential effect of climate change on the global carbon cycle. A soil profile data set(n = 1490) from the Second National Soil Survey of China conducted from 1979 to 1994 was used to explore the relationships of SOC density with mean annual temperature(MAT) and mean annual precipitation(MAP) in six soil regions and eight paddy soil subgroups. Results showed that SOC density of paddy soils was negatively correlated with MAT and positively correlated with MAP(P < 0.01). The relationships of SOC density with MAT and MAP were weak and varied among the six soil regions and eight paddy soil subgroups. A preliminary assessment of the response of SOC in Chinese paddy soils to climate indicated that climate could lead to a 13% SOC loss from paddy soils. Compared to other soil regions, paddy soils in Northern China will potentially more sensitive to climate change over the next several decades. Paddy soils in Middle and Lower Yangtze River Basin could be a potential carbon sink. Reducing the climate impact on paddy soil SOC will mitigate the positive feedback loop between SOC release and global climate change. 展开更多
关键词 soil organic carbon paddy soils mean annual temperature mean annual precipitation climate change
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Brayton Power Cycles for Electricity Generation from Fusion Reactors
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作者 J.l. Linares L.E. Herranz +1 位作者 B.Y. Moratilla I.P. Serrano 《Journal of Energy and Power Engineering》 2011年第7期590-599,共10页
Brayton power cycles for fusion reactors have been investigated, using Helium in classical configurations and CO2 in a recompression layout. Thermal sources from the reactor have strongly constrained the cycle configu... Brayton power cycles for fusion reactors have been investigated, using Helium in classical configurations and CO2 in a recompression layout. Thermal sources from the reactor have strongly constrained the cycle configurations, hindering use of a recuperator in Helium cycles and conditioning the outlet turbine temperature in CO2 ones. In both cycles, it is possible to take advantage of the exhaust thermal energy by coupling the Brayton to a Rankine cycle, with an organic fluid in the helium case (iso-butane has been investigated) and steam in the CO2 case. The highest efficiency achieved with Helium cycle is 38.5% using Organic Rankine Cycle and 32.6% with Helium alone. The efficiency changes from 46.7% using Rankine cycle to 41% with CO2 alone. The Helium cycle is highly sensitive to turbine efficiency and in a moderate way to compressor efficiency and pressure drops, being nearly insensitive to thermal effectiveness in heat exchangers. On the other hand, CO2 is nearly insensitive to all the parameters. 展开更多
关键词 Brayton cycles fusion technology CO2 recompression cycles organic Rankine cycles.
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中国区域陆地生态系统碳收支综合研究的科技需求与重要科学问题 被引量:14
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作者 王秋凤 刘颖慧 +3 位作者 何念鹏 方华军 伏玉玲 于贵瑞 《地理科学进展》 CSCD 北大核心 2012年第1期78-87,共10页
陆地生态系统碳收支及其循环过程机制研究一直是全球气候变化的成因分析、变化趋势预测、减缓和适应对策分析等领域的热点,受到科技界和国际社会的广泛关注。本文在简要回顾中国陆地生态系统碳收支及其循环过程研究领域的发展历史,总结... 陆地生态系统碳收支及其循环过程机制研究一直是全球气候变化的成因分析、变化趋势预测、减缓和适应对策分析等领域的热点,受到科技界和国际社会的广泛关注。本文在简要回顾中国陆地生态系统碳收支及其循环过程研究领域的发展历史,总结各个发展阶段主要特征的基础上,讨论了开展中国区域陆地生态系统碳收支综合研究的科技需求和社会需求,评述了中国在相关领域研究中存在的主要问题,探讨了当前的科学研究前沿领域及其关键科学问题。本文指出,现阶段中国开展区域尺度陆地生态系统碳收支及其循环过程机制综合研究工作不仅是提升中国生态系统生态学、地球系统科学与全球变化科学的创新能力的科技发展需求,更是中国参与应对全球气候变化国际合作、改进生态系统管理、保障生态安全的社会经济发展需求。同时还指出,中国现阶段在该领域的研究工作还缺乏各类生态系统碳收支的实际调查数据,缺乏国家尺度碳收支科学数据的整合,缺乏可用于碳收支计量与综合评估的模型工具,也没有形成国家层次的碳源汇计量、评估、认证及决策分析信息系统平台。本文通过国内外科技发展的分析认为,中国在该领域的研究工作,应在大力发展陆地生态系统碳收支和碳汇功能的定量监测、评价和认证的方法与技术基础上,重点关注并前瞻性地开展陆地生态系统碳-氮-水循环过程耦合关系及其对全球气候变化的响应与适应、碳-氮-磷生态化学计量学特征及其环境影响、碳-氮-水耦合循环过程的生物调控机制等前沿领域,以提高中国生态系统与全球变化科学研究水平,为国家的生态系统与温室气体管理提供基础理论、科学知识和先进技术的储备。 展开更多
关键词 收支与循环 汇功能 --耦合循环 增汇技术与潜力 陆地生态系统 中国
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Estimates of net primary productivity and actual evapotranspiration over the Tibetan Plateau from the Community Land Model version 4.5 with four atmospheric forcing datasets
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作者 Shan Lin Kewei Huang +5 位作者 Xiangyang Sun Chunlin Song Juying Sun Shouqin Sun Genxu Wang Zhaoyong Hu 《Journal of Plant Ecology》 SCIE CSCD 2024年第4期70-89,共20页
The accuracy of the simulation of carbon and water processes largely relies on the selection of atmospheric forcing datasets when driving land surface models(LSM).Particularly in high-altitude regions,choosing appropr... The accuracy of the simulation of carbon and water processes largely relies on the selection of atmospheric forcing datasets when driving land surface models(LSM).Particularly in high-altitude regions,choosing appropriate atmospheric forcing datasets can effectively reduce uncertainties in the LSM simulations.Therefore,this study conducted four offline LSM simulations over the Tibetan Plateau(TP)using the Community Land Model version 4.5(CLM4.5)driven by four state-of-the-art atmospheric forcing datasets.The performances of CRUNCEP(CLM4.5 model default)and three other reanalysis-based atmospheric forcing datasets(i.e.ITPCAS,GSWP3 and WFDEI)in simulating the net primary productivity(NPP)and actual evapotranspiration(ET)were evaluated based on in situ and gridded reference datasets.Compared with in situ observations,simulated results exhibited determination coefficients(R2)ranging from 0.58 to 0.84 and 0.59 to 0.87 for observed NPP and ET,respectively,among which GSWP3 and ITPCAS showed superior performance.At the plateau level,CRUNCEP-based simulations displayed the largest bias compared with the reference NPP and ET.GSWP3-based simulations demonstrated the best performance when comprehensively considering both the magnitudes and change trends of TP-averaged NPP and ET.The simulated ET increase over the TP during 1982-2010 based on ITPCAS was significantly greater than in the other three simulations and reference ET,suggesting that ITPCAS may not be appropriate for studying long-term ET changes over the TP.These results suggest that GSWP3 is recommended for driving CLM4.5 in conducting long-term carbon and water processes simulations over the TP.This study contributes to enhancing the accuracy of LSM in water-carbon simulations over alpine regions. 展开更多
关键词 land surface model carbon cycle water cycle high altitude Community Land Model version 4.5
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