Measuring the Effect of Foreign Direct Investment on CO2 Emissions in Laos

This paper aims to explore the determinants of CO₂ emissions in Laos by accounting for the significant role played by foreign direct investment (FDI) in influencing CO₂ emissions during the period 1990-2017. We apply a Johansen co-integration testing approach to investigate the presence of co-integration, and the empirical findings underscore the presence of a long-run co-integration relationship between CO₂ emissions, FDI, per capita GDP, and industrial structure. We also employ an error-correcting model to examine the short-term dynamic effect of FDI on CO₂ emissions. The empirical results show that FDI has a significant short-term dynamic effect on changes in CO₂ emissions, indicating that the relationship between FDI and CO₂ emissions is an inverted U-shaped curve. This is a validation of the EKC. Changes of FDI, per capita GDP, and industrial structure increase CO₂ emissions. Based on the analysis results, this paper puts forward policy suggestions emphasizing the need for both Laotian policymakers and Chinese investors to improve eco-environmental quality.     

基于可持续发展的绿色广东制度建设的动力机制

绿色广东建设的内涵丰富,其根本核心是基于可持续发展的制度创新。制度创新有利于克服科技创新面临的外部性障碍和风险,是实现从传统经济向循环经济模式转变的关键。在分析广东省制度创新的优势与不足的基础上,揭示推动绿色广东建设的动力机制,提出绿色广东制度创新的对策。具体通过建立资源环境有偿使用机制、环境容量分配及排污权交易等机制,探索生态补偿机制的市场化运作,并在广东率先培育中国式的环境非政府组织(NGO),建立享有环境权益的公众参与机制,形成政府、市场、公众等三方参与的激励约束兼容机制。     

河口海岸GIS时空过程可视化表达

河口海岸带中一些随时间变化的三维海洋现象(如涡漩、锋面、水团等)的时空建模与可视化表达是海洋地理信息系统(MGIS)发展的一大难题。基于流体建模与可视化AVIZO Green技术,针对海洋连续场中的三维海洋现象,提出了基于特征的时空三域动态识别技术,设计并实现了面向主题应用的时空四维GIS可视化框架,能够有效表达三维海洋现象。以长江口海岸带涡漩、冲淡水、羽状锋和盐跃层为例进行三维动态可视模拟,直观再现了object-like型和field-like型海洋现象的时空演绎过程,为海洋现象仿真研究,尤其是多维、动态、边界模糊的复杂海洋现象的有效表达提供了一种新思路和方法。     

基于生态系统的海洋综合管理研究 ——以美国大沼泽湿地项目为例

基于生态系统的海洋综合管理是海洋管理的新理念和新模式,其倡导从海洋生态系统角度开展环境资源保护,并以促进海洋生态系统与人类开发活动的协调可持续发展为终极目标。美国大沼泽湿地项目是基于生态系统的海洋综合管理的经典范例。基于生态系统的海洋综合管理的核心理念是将整个生态系统纳入海洋综合管理范畴,颠覆传统的单一对象保护理念,实现海洋生态保护与人类生存发展协调可持续。美国大沼泽湿地项目采用了基于生态系统的海洋综合管理理念,将整个大沼泽湿地视为一个整体生态系统,实现联邦政府、州政府和社会组织协作,合力促进大沼泽湿地的绿色生态可持续发展。美国大沼泽湿地项目全面贯彻基于生态系统的海洋综合管理理念,采用联合管理模式,重视水资源环境治理取得一定成效,但也暴露出管理模式有待改进、公众宣传参与不到位、区域间联系不紧密等问题。     

黄土高原粮食生产空间重构过程中的生态系统服务权衡——以陕北榆林市为例

粮食生产空间重构集中了土地系统变化的主要矛盾,探索粮食生产空间重构过程中的生态系统服务权衡变化有利于明确粮食安全、生态修复与经济发展之间的矛盾,从而推进区域生态文明建设和高质量发展.采用生态系统服务评估模型及均方根偏差法,对2000—2018年陕北榆林市粮食生产空间重构过程中的固碳、食物供给、土壤保持和产水服务及其权衡...     

一类分数阶差分方程边值问题多重正解的存在性

研究一类带有分数阶边界条件的分数阶差分方程多重正解的存在性.分析该方程的Green函数的性质,引入上、下解的概念,并利用Guo-Krasnosel'skii不动点定理和上、下解的方法,分别建立该方程存在正解的充分条件,最后利用Legget-Williams不动点定理,讨论该方程多重正解的存在性.     

有航速浮体时域分析的混合边界元法

给出了一种联合瞬态格林函数和Rankine源进行有航速浮体时域水动力分析的混合——边界元方法。在三维混合边界元方法中,通过一个匹配面将流体域划分为内域和外域,在内域中使用Rankine源以模拟直壁或非直壁船体及线性或非线性自由面条件,在外域中使用瞬态格林函数以满足自由面条件和远方辐射条件。使用该方法计算了一个有航速潜没圆球的波浪力,和解析结果的比较证明了该方法的正确性。进一步给出了一个有航速Wigley船的水动力结果,计算结果稳定,没有外传波向内反射的现象发生。     

Seasonal variability of Holocene climate: a palaeolimnological study on varved sediments in Lake Jues (Harz Mountains, Germany)

Studies combining sedimentological and biological evidence to reconstruct Holocene climate beyond the major changes, and especially seasonality, are rare in Europe, and are nearly completely absent in Germany. The present study tries to reconstruct changes of seasonality from evidence of annual algal successions within the framework of well-established pollen zonation and ¹⁴C-AMS dates from terrestrial plants. Laminated Holocene sediments in Lake Jues (10°20.7′ E, 51°39.3′ N, 241 m a.s.l.), located at the SW margin of the Harz Mountains, central Germany, were studied for sediment characteristics, pollen, diatoms and coccal green algae. An age model is based on 21 calibrated AMS radiocarbon dates from terrestrial plants. The sedimentary record covers the entire Holocene period. Trophic status and circulation/stagnation patterns of the lake were inferred from algal assemblages, the subannual structure of varves and the physico-chemical properties of the sediment. During the Holocene, mixing conditions alternated between di-, oligo- and meromictic depending on length and variability of spring and fall periods, and the stability of winter and summer weather. The trophic state was controlled by nutrient input, circulation patterns and the temperature-dependent rates of organic production and mineralization. Climate shifts, mainly in phase with those recorded from other European regions, are inferred from changing limnological conditions and terrestrial vegetation. Significant changes occurred at 11,600 cal. yr. BP (Preboreal warming), between 10,600 and 10,100 cal. yr. BP (Boreal cooling), and between 8,400 and 4,550 cal. yr. BP (warm and dry interval of the Atlantic). Since 4,550 cal. yr. BP the climate became gradually cooler, wetter and more oceanic. This trend was interrupted by warmer and dryer phases between 3,440 and 2,850 cal. yr. BP and, likely, between 2,500 and 2,250 cal. yr. BP.