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991.
景观尺度、过程及格局(LSPP)研究的内涵及特点   总被引:1,自引:0,他引:1  
王让会 《热带地理》2018,38(4):458-464
景观尺度、过程与格局(LSPP)及其相互作用是景观生态学研究的核心内容。在分析景观尺度及效应、景观生态过程、景观格局及变化的基础上,凝练出了LSPP一体化理念的主要特征,并探索了LSPP中各要素之间的耦合关系。研究表明:LSPP一体化具有一定的理论价值,景观时空尺度是LSPP的重要基础,LSPP体现了景观过程及其生态效应。景观生态研究所涉及的结构、功能、动态与LSPP一体化等的理论与应用问题,随着新时代生态环境的复杂化,在情景模拟技术、大数据挖掘技术,以及生态物联网等技术支撑下,促进了景观生态学机理研究与应用范式的拓展与深化,对于当前区域发展与生态文明建设具有重要指导意义。  相似文献   
992.
城市化与生态环境关系研究热点与前沿的图谱分析   总被引:2,自引:1,他引:1  
城市化与生态环境关系的相关研究已成为人地关系地域系统研究的热点问题与前沿领域。基于1999-2016年WOS和CNKI数据库中城市化与生态环境相关研究主题的文献样本数据,利用Excel、SPSS和CiteSpace软件,通过学科共现分析、文献共被引分析、突现词探测、关键词共现分析和多维尺度分析等,系统梳理了城市化与生态环境关系研究领域的前沿、知识基础、现状热点与发展动态,结果显示:①研究前沿从城市化与生态环境系统的单一要素逐渐走向多要素综合研究,由单向作用逐步转向系统间和系统外部的相互作用研究;②快速城市化背景下土地利用变化、生态系统服务、气候变化、景观格局和生态环境效应等方面已成为近期研究热点;③国内相关研究缺乏在多尺度视角下利用新技术集成方法进行跨学科的综合性研究。最后,提出了城市化与生态环境的基本格局—过程—机理、跨区域的多尺度研究、城市化的生态环境效应及其影响因素、快速城市化过程中生态环境问题形成与优化调控、城市化与生态环境的可持续发展等领域的研究展望。  相似文献   
993.
汤青  李扬  陈明星  徐勇 《地理科学进展》2018,37(8):1022-1030
可持续生计理论方法不仅可以应用于城市务工的半城镇化农民,服务于有序推进中国的城镇化,而且可广泛应用于中国西部农村地区和农户尺度的研究,服务于农村可持续发展。本文首先梳理了当前可持续生计的概念及分析框架,并基于半城镇化农民可持续生计与农村可持续发展,从地理学的综合视角提出了一个适应于中国实证研究的理论分析框架。然后依托国家自然科学基金青年科学基金项目“半城镇化农民生计状态评估及市民化阻滞因素与政策调控”,梳理了可持续生计的国际国内研究进展以及半城镇化农民市民化与农村地区可持续发展的中国实证研究成果。最后提出了未来的研究展望,包括半城镇化农民市民化与农村地区可持续发展的联动研究,半城镇化农民市民化转变的主观意愿与客观阻滞因素综合研究,半城镇化农民与农村发展作用机理及其市民化效应,可持续生计与农村可持续发展的集成研究。  相似文献   
994.
The first step to defining the rights, responsibilities and interests of stakeholders and constructing a compensation mechanism is to identify the stakeholders and clarify their mutual relationships. Nature reserves are complex ecosystems involving nature, the economy and society. There exists a conflict between the public welfare benefits of ecological conservation and the private gains to be realized from social and economic development. There also exist in a nature reserve complex relationships among stakeholders, involving the utilization of ecological resources, ecological conservation and ecological-economic interests. The introduction of tourism brings substantial changes to the existing stakeholder benefit structure in a nature reserve. The implementation of tourism ecological compensation (tourism payment for ecological service) is a process for redefining the distribution of rights, responsibilities and profits among stakeholders and it is also an essential way to balance the interests of the stakeholders. This paper uses a case study of Sanya Coral Reef National Nature Reserve in China to examine the characteristics of stakeholders and analyze their interests. According to the method for defining basic attributes proposed by Mitchel and other scholars, in cases of tourism ecological compensation, stakeholders can be classified as definitive stakeholders, expectant stakeholders and latent stakeholders. This paper applies these classifications and then analyzes the relationships between the rights and responsibilities of these stakeholders and how these change after the implementation of compensation. Additionally, based on the impact compensation has on different stakeholders, changes in the relationships can be analyzed and the structure of the stakeholders can be modelled. This case study of the Sanya Coral Reef National Nature Reserve illustrates the operationalization of a new mechanism for tourism ecological compensation. The paper illustrates a method for coordinating the relationships among the stakeholders involved with this national-level nature reserve.  相似文献   
995.
Analyzing the spatial and temporal properties of information flow with a multi-century perspective could illuminate the sustainability of human resource-use strategies. This paper uses historical and archaeological datasets to assess how spatial, temporal, cognitive, and cultural limitations impact the generation and flow of information about ecosystems within past societies, and thus lead to tradeoffs in sustainable practices. While it is well understood that conflicting priorities can inhibit successful outcomes, case studies from Eastern Polynesia, the North Atlantic, and the American Southwest suggest that imperfect information can also be a major impediment to sustainability. We formally develop a conceptual model of Environmental Information Flow and Perception (EnIFPe) to examine the scale of information flow to a society and the quality of the information needed to promote sustainable coupled natural-human systems. In our case studies, we assess key aspects of information flow by focusing on food web relationships and nutrient flows in socio-ecological systems, as well as the life cycles, population dynamics, and seasonal rhythms of organisms, the patterns and timing of species’ migration, and the trajectories of human-induced environmental change. We argue that the spatial and temporal dimensions of human environments shape society’s ability to wield information, while acknowledging that varied cultural factors also focus a society’s ability to act on such information. Our analyses demonstrate the analytical importance of completed experiments from the past, and their utility for contemporary debates concerning managing imperfect information and addressing conflicting priorities in modern environmental management and resource use.  相似文献   
996.
西北农牧交错带生态环境脆弱,区位特殊性和生态重要性使其在我国社会经济发展和生态环境保护方面具有重要战略意义。通过对该区域进行土地利用优化配置,使有限的土地资源支撑起生态环境保护和经济发展的重任是本文的出发点。多目标遗传算法和FLUS模型的应用可以从多方面(数量结构、空间布局、综合效益)完善土地利用优化配置,为土地利用优化配置提供更多的选择方案。本文选用多目标遗传算法和FLUS模型对该区域进行2025年的土地利用变化模拟,通过设置自然发展、生态保护优先、经济发展优先、生态-经济均衡4种情景,探讨了如何在兼顾生态环境保护与社会经济发展的情况下进行土地利用的优化配置。结果表明,基于生态-经济均衡情景下的优化方案,土地利用类型的数量结构和空间布局更为合理,其综合效益优于另外3种情景。该情景在合理限制经济发展速度的前提下,使生态建设获得稳定发展,其经济效益较生态保护优先情景下增长了8.96%,生态效益较经济发展优先情景下增长了0.77%,在生态保护与经济发展2种目标之间达到平衡,为西北农牧交错带的土地利用规划提供了决策辅助。  相似文献   
997.
近年来,我国城镇突出的生态环境问题受到社会广泛关注,作为生态环境保护工作的重要组成部分,随着城镇化的快速发展,城镇生态环境监测任务也越来越重、要求越来越高,对结合空间信息的天地一体综合监测的需求非常迫切,急需建立其技术体系,以指导城镇生态环境综合监测工作的开展。本文面向城镇生态环境综合监测的需求,从城镇污染气体、水体水质、生态资源3个方面出发,通过梳理城镇生态环境综合监测中的关键科学技术问题,结合开展的关键技术攻关研究,经过分析论证,构建了城镇生态环境综合监测技术体系框架、指标体系框架以及标准体系框架。在此基础上,根据遥感数据特点及国家生态环境监测需求,提出城镇生态环境综合监测业务应用方案,为国家和省市地方下一步有效开展城镇生态环境监测、管理等工作提供重要指导和支撑。  相似文献   
998.
为实现“一带一路”区域可持续发展,我国倡导绿色、低碳、循环、可持续的生产生活方式,建设绿色“一带一路”。遥感技术在生态环境监测与评价方面具有重要作用。本文以“一带一路”区域中国援建的水电站工程为研究对象,基于陆地系列卫星(Landsat)、哨兵2号(Sentinel-2)等遥感对地观测数据,利用决策树与缓冲区分析等方法,从水电站库区概况、水电站对植被生长状况与生态资源影响等方面,开展“一带一路”区域水电站项目建设对当地经济发展和生态环境影响的遥感监测及分析。本文首先根据遥感影像与DEM确定库区及库容,结合最小外接正方形面积比及平均宽度等指标确定各水电站缓冲区类型和范围。利用NDWI及NDVI构建决策树模型,提取各缓冲区土地利用类型,分为水体、林地、草地、耕地和其它5类;结合区域植被覆盖度,估算库区生态占用并对水电站建成前后的土地利用类型和植被变化进行分析。研究结果表明:① “一带一路”沿线10座水电站造成的生态损失与库区面积呈正相关,不同工程间,在水体、林地、草地、耕地和其它方面的损失面积大小存在较大差异;② 土地利用类型与植被覆盖度年均变化幅度约为0.35%、1.27%,水电站修建对周边生态资源与植被生长状况影响较小,同时在植被覆盖度较低的地区水电站的修建会明显改善周边环境;③ 各水电站周边的植被覆盖度差异较大,大部分水电站周边植被生长状况良好;④ 水电站建设始终坚持工程建设与环境保护并重,从施工设计到水电站后期维护期间,积极采取环保措施,减少占用,保护生物多样性,生态风险防范得当;⑤ 水电站提供了优质的清洁能源,促进了当地经济和社会发展。  相似文献   
999.
山西炼焦煤资源与开发利用现状分析   总被引:1,自引:0,他引:1  
山西省炼焦煤资源丰富、优势突出;资源分布广泛,煤类分布规律明显;开发技术条件较好;优质炼焦煤资源稀缺,比较适宜炼焦的资源大约在900亿t,低灰、低硫的优质炼焦煤大约占炼焦煤查明资源储量的12%,而优质的焦煤和肥煤仅占2.5%;查明资源总体利用水平低,但低硫煤资源占用率高;勘探程度较低,探明的资源储量少;查明资源总体利用水平低,经济可采储量少。通过分析山西炼焦煤炭资源开发利用现状,认为确保山西炼焦煤经济的可持续发展,必须加强炼焦煤炭资源的规划与管理,提高炼焦煤资源保障能力,保护与节约并重,合理开发利用炼焦煤资源。  相似文献   
1000.
This report presents mineralogical, geochemical and isotopic data on samples obtained using the Benthic Multi‐coring System (BMS) to drill a submarine hydrothermal deposit developed in a caldera on the summit of the Suiyo Seamount in the Izu–Bonin Island Arc, south of Japan. This deposit is regarded as the first example of Kuroko‐type sulfide mineralization on a volcano at the volcanic front of an island arc. The mineralization and hydrothermal alteration below the 300 × 150‐m area of active venting was investigated to depths of 2–9 m below the sea floor. Drilling beneath the area of active venting recovered a sequence of altered volcanic rocks (dacite lavas, pyroclastic rocks of dacite–rhyolite compositions and pumice) associated with sulfide veining and patches/veins of anhydrite. No massive sulfide was found, however, and the subsea‐floor mineralization to 10 m depth is dominated by anhydrite and clay minerals with some sulfides. Sulfide‐bearing samples contained high Au (up to 42 ppm), Ag (up to 263 ppm), As (up to 1550 ppm), Hg (up to 55 ppm), Sb (up to 772 ppm), and Se (up to 24 ppm). Electron probe microanalyzer indicated that realgar, orpiment, and mimetite were major As‐bearing minerals. The sulfides were also characterized by high Zn (>10%) compared to Cu (<6.3%) and Pb (<0.6%). The δ202Hg/198Hg, δ202Hg/199Hg and δ202Hg/200Hg of the sulfide‐bearing dacite samples and a sulfide chimney decreased with increasing Hg/Zn concentration ratio. The variation of the δ202Hg/198Hg ranged from ?2.8 to +0.5‰ to relative to S‐HG02027. The large range of these δ202Hg/198Hg was greater than might be expected for such a heavy element and may be due to a predominance of kinetic effects. The variation of δ202Hg/198Hg of sulfide‐bearing dacite samples suggested that light Hg isotope in the vapor mixed with oxygenated seawater near sea floor during mineralization. Lead isotope ratios of the sulfide were very similar to those of the dacite lava, suggesting that lead is of magmatic origin. The 87Sr/86Sr ratio (0.70872) of anhydrite was different from that of the dacite lava, and suggests an Sr derivation predominantly from seawater. Hydrothermal alteration of the dacite in the Suiyo hydrothermal field was characterized by Fe‐sulfides, anhydrite, barite, montmorillonite, chlorite/montmorillonite mixed‐layer minerals, mica, and chlorite with little or no feldspar or cristobalite. Hydrothermal clay minerals changed with depth from montmorillonite to chlorite/montmorillonite mixed‐layer minerals to chlorite and mica. Hydrogen isotope ratios of chlorite/montmorillonite and mixed‐layer, mica‐chlorite composites obtained below the active venting sites ranged from ?49 to ?24‰, suggesting seawater as the dominant fluid causing alteration. Oxygen isotope ratios of anhydrite ranged from 9.2 to 10.4‰ and anhydrite formation temperatures were calculated to be 188–207°C. Oxygen isotope ratios ranged from +5.2 to +9.2‰ for montmorillonite, +3.2 to +4.5‰ for chlorite/montmorillonite mixed‐layer minerals, and +2.8 to +3.8‰ in mixtures of chlorite and mica. The formation temperatures of montmorillonite and of the chlorite–mica mixture were 160–250°C and 230–270°C, respectively. The isotope temperatures for clay minerals (220–270°C) and anhydrite (188°C) were significantly lower than the borehole temperature (308.3°C) measured just after the drilling, suggesting that temperature at this site is now higher than when clay minerals and anhydrite were formed.  相似文献   
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