马克思自然观的生态意义

摘要：当代社会，生态问题已成为全球性的问题。但早在马克思生存的时代就已经初露端倪，马克思对此进行了详细的阐述并且提出了解决途径。     

浅析松花湖渔业资源保护

通过多年实地调研,认为拦网养殖、湖滩地种植、过度捕捞、沿湖城镇生活污水污染等是渔业资源不断减少主要原因,并根据实际情况提出防治对策。     

严惩环境污染犯罪观念之反思

目前,中国重大环境污染事故频发,严重危害了公民居住的环境甚至是公共安全,在社会上引起了广泛影响,民众要求严惩环境污染犯罪的观念也日益盛行。从客观上来讲,严惩环境污染犯罪有一定的意义,但此种观念的蔓延也可能带来一系列的副作用,因此有必要对此种观念进行深刻反思。通过对环境污染犯罪进行综合分析可以发现,导致此类犯罪的原因是多方面的,因而预防该类犯罪的方法也应当是多元的,仅仅严惩是起不到防治环境污染犯罪效果的。     

Application of an Artificial Sea Salt Solution to Determine Acute Toxicity of Herbicides to Proisotoma minuta (Collembola)

The acute toxicity test is described in this experiment where the Collembola species Proisotoma minuta was exposed to herbicides in an artificial sea salt solution for seven days. The salt solution did not prohibit the insects' reproduction system. The seven day LD₅₀ values for trifluralin, pendimethalin, metolachlor, prometryn, paraquat, atrazine, fluometuron, and diuron were 3.48, 10.4, 12.4, 13.0, 23.1, 33.4, 250, and 711 mg L^?1, respectively. A good correlation between toxicity of the compounds and their lipophilicity and vapor pressure was recorded in this study.     

基坑围护结构的内力和变形的预测方法研究

为了利用土体水平抗力系数的比例系数m来有效预测基坑围护结构的内力和变形,依据弹性地基梁原理,利用大型数学软件MATLAB编制了计算程序,对基坑围护结构的内力和变形进行预测,并依托某深基坑工程围护结构的实测内力和变形数据对预测的内力和位移进行了验证。结果表明,根据弹性地基梁原理预测的基坑围护结构内力和变形随基坑开挖的变化与实测结果吻合较好。     

浅析辽河流域水环境管理现状及改善措施

辽河流域是我国北方重要的河流型流域,水环境污染问题突出。文章从水环境管理体制、水污染控制方式、水生态安全管理、预警监控4个方面剖析了辽河流域水环境管理现状,并提出针对性的改善措施,对促进辽河流域水环境管理能力提高具有积极的实际意义。     

有机-无机纳米聚硅氧烷涂料的耐蚀性研究

目的研究有机-无机纳米聚硅氧烷涂料的耐蚀性。方法将涂层试样制作划痕后,采用盐雾试验方法和盐溶液周浸试验方法进行加速腐蚀试验,采用最大剥落值对涂层剥落程度进行量化考核。结果获得了4种涂料在试验环境下的腐蚀失效模式、失效过程、失效程度、以及涂层损伤随加速腐蚀时间的变化规律等方面的试验数据。结论在盐雾试验中,涂层的失效模式主要是剥落,盐溶液周浸试验主要是剥落和鼓泡。在盐雾腐蚀环境下,3#涂料耐蚀性最佳,在周浸腐蚀环境下1#涂料耐蚀性最佳。采用最大剥落值对涂层的剥落程度进行量化考核是可行的。     

亚麻二粗加工企业的除尘系统研究与应用

论述了有关亚麻二粗加工企业的除尘系统设计问题。     

Boundary work in climate policy making in Brazil: Reflections from the frontlines of the science-policy interface

Despite challenges to the authority and legitimacy of science as a neutral representation of the world, expert advisors are playing an increasingly central role in environmental policy-making in both the Global North and South. This article explores the science-policy interface, based on the experience of the main author as a scientist and policy-maker at FEAM, a state-level environmental agency in Brazil. Contributing to the literature on boundary objects and organizations, the article details the practices necessary to manage the relationship between political and scientific norms in the development of the regional Climate and Energy Plan (CEP) for the state of Minas Gerais. To sustain the role of FEAM as a boundary organization mediating between political and scientific demands, a team of scientists and policy-makers had to perform different types of boundary work in a closely connected manner. It was necessary to actively frame climate change as an economic problem, and structure its solution in terms of mitigation mechanisms. Responding to changes in the national and international political context, FEAM reframed climate change from mitigation into largely an adaptation issue that could lead to win-win solutions as to attain saliency and avoid insurmountable political obstacles for its approval. Based on this experience, the article argues that the performance of boundary objects and organizations in the science-policy interface not only requires an ability to bring ‘truth to power’ but to also the capacity to sense, anticipate and avoid political obstacles. For this reason even though boundary organizations provide a breeding ground for institutional learning it is an unsuitable location for scientific or political revolutions.     

SIMULATING THREE-DIMENSIONAL GROUND WATER RESPONSE IN A SMALL MOUNTAINOUS WATERSHED1

ABSTRACT: Snowmelt from deep mountainous snowpacks is seldom rapid enough to exceed infiltration rates; thus, the source of streamflow in many mountainous watersheds is snowmelt recharge through shallow ground water systems. The hydrologic response and interaction between surface and sub-surface flow processes in these watersheds, which is controlled by basin structure, the spatial distribution of snowmelt, and the hydrogeology of the subsurface, are not well understood. The purpose of this study was to test a three-dimensional ground water model using simulated snowmelt input to simulate ground water response to spatially distributed snowmelt on the Upper Sheep Creek Watershed located within the Reynolds Creek Experimental Watershed in Southwestern Idaho. The model was used to characterize the mountainous aquifer and to delineate the subsurface flow mechanisms. Difficulty in finding a reasonable combination of grid spacing and time stepping within the model was encountered due to convergence problems with the Picard solution to the non-linear variably saturated ground water flow equations. Simulation results indicated that flow may be either unconfined or confined depending on inflow rate and hydrogeologic conditions in the watershed. The flow mechanism had a much faster response time when confined flow occurred. Response to snowmelt from a snow drift approximately 90 m away took only a few hours when flow was confined. Simulated results showed good agreement with piezometer measurements both in magnitude and timing; however, convergence problems with the Picard solution limited applicability of the model.