Economic development and environmental protection: an ecological economics perspective

This paper argues on both theoretical and empirical grounds that, beyond a certain point, there is an unavoidable conflictbetween economic development (generally taken to mean 'materialeconomic growth') and environmental protection. Think for a moment of natural forests, grasslands, marine estuaries, salt marshes, and coral reefs; and of arable soils, aquifers, mineraldeposits, petroleum, and coal. These are all forms of 'natural capital' that represent highly-ordered self-producing ecosystemsor rich accumulations of energy/matter with high use potential (low entropy). Now contemplate despoiled landscapes, eroding farmlands, depleted fisheries, anthropogenic greenhouse gases,acid rain, poisonous mine tailings and toxic synthetic compounds.These all represent disordered systems or degraded forms of energy and matter with little use potential (high entropy). The main thing connecting these two states is human economic activity. Ecological economics interprets the environment-economyrelationship in terms of the second law of thermodynamics. The second law sees economic activity as a dissipative process. Fromthis perspective, the production of economic goods andservices invariably requires the consumption of available energy and matter. To grow and develop, the economynecessarily 'feeds' on sources of high-quality energy/matter first produced by nature. This tends to disorder and homogenizethe ecosphere, The ascendance of humankind has consistently been accompanied by an accelerating rate of ecological degradation, particularly biodiversity loss, the simplificationof natural systems and pollution. In short, contemporary political rhetoric to the contrary, the prevailing growth-oriented global development paradigm is fundamentally incompatible with long-term ecological and social sustainability. Unsustainability is not a technical nor economic problem as usually conceived, but rather a state of systemic incompatibilitybetween a economy that is a fully-contained, growing, dependent sub-system of a non-growing ecosphere. Potential solutions fly inthe face of contemporary development trends and cultural values.     

Selecting Socio-Economic Metrics for Watershed Management

The selection of social and economic metrics to document baseline conditions and analyze the dynamic relationships between ecosystems and human communities are important decisions for scientists, managers, and watershed citizens. A large variety of social and economic data is available but these have limited use without theoretical frameworks. In this paper, several frameworks for reviewing social-ecosystem relations are offered, namely social sanctions, sense of place, civic structure, and cultural differences. Underlying all of these frameworks are attitudes, beliefs, values, and norms that affect which questions are asked and which indicators are chosen. Much work and significant challenges remain in developing a standard set of spatially based socio-economic metrics for watershed management.     

东南大陆岩石圈板块地体构造

东南大陆的地质构造模型,具有欧亚大陆边缘向洋增生的独特形式。除外来地体之外,或以扩张、地幔上涌,洋壳向大陆地壳转化,并不断向洋增生;或是大陆分裂,地幔柱——热点物质不断注入变薄和破裂了的地壳,形成区域性新的生长构造层,构造岩浆地质体表现为有独特属性的“A型”花岗岩和流纹岩链。这些高DI值的富硅富碱富钠质岩石,出现在欧亚大陆边缘的重力梯度带上。裂解带的地壳结构模式是上地壳存在着重力不稳定的硅铝低速带;中地壳有洋——陆过渡型地壳的“类裂谷型”结构,P波速度为6.3～6.4km/s的中间壳层;在下地壳下部有速度为7.0～7.4km/s的壳——幔混合型高速层;随着“异常”的上地幔的形成,有大范围的热活动和壳——幔边界穹窿,穹窿的地盖比正常区为为薄。由于化学库和化学边界层的横向不连续,可划分出古老基底和后期地质发展史完全迥异的两个亚板块;和以壳层(或幔层)断裂为边界特点的八个地体;一个以分裂为主,并具热点径迹的最新生长构造层的扩张——裂解构造岩浆地体。     

An overview on industrial waste management in China

Ａｎｏｖｅｒａｌｌｄｅｓｃｒｉｐｔｉｏｎｏｆｉｎｄｕｓｔｒｉａｌｗａｓｔｅｗａｓｇｉｖｅｎｆｒｏｍｇｅｎｅｒａｔｉｏｎ；ｔｒｅａｔｍｅｎｔ，ｄｉｓｐｏｓａｌａｎｄｅｍｉｓｓｉｏｎａｎｄｃｏｍｐｒｅｈｅｎｓｉｖｅｕｔｉｌｉｚａｔｉｏｎ．Ｉｎｓｐｉｔｅｏ...     

Quantitative structure - activity study on the reductivedehalogenation potency of the halogenated aromatics

Ｑｕａｎｔｉｔａｔｉｖｅｓｔｒｕｃｔｕｒｅ－ａｃｔｉｖｉｔｙｓｔｕｄｙｏｎｔｈｅｒｅｄｕｃｔｉｖｅｄｅｈａｌｏｇｅｎａｔｉｏｎｐｏｔｅｎｃｙｏｆｔｈｅｈａｌｏｇｅｎａｔｅｄａｒｏｍａｔｉｃｓＨｕａｎｇＱｉｎｇｇｕｏ；ＷａｎｇＬｉａｎｓｈｅｎｇ；Ｈａｎ...     

寻找紧缺的银矿资源——地质工作者的急迫使命

由于近二十年来全世界工业的快速发展 ,银的用途益发广泛 ,白银需求量迅猛增加 ,它不仅是我国紧缺的矿产资源 ,而且已成为世界市场上的走俏商品 ,全世界已连续九年需大于供 ,九年累计缺银 1 0亿盎司 ,并且缺口越来越大。专家们预测 :到 1 998年底全世界库存的银锭消耗殆尽。我国前几年有 1 / 2 -1 / 3的白银靠进口 ,1 997年还进口白银 1 55吨。因而 ,银价剧烈上扬 ,从 1 996年的 4美元 /盎司 ,涨到 1 998年 2月份的 7.81美元 /盎司。与白银相反 ,近两年黄金供远过于求 ,1 997年全世界多出 3 93吨 ,故金价急剧下跌 ,从 1 996年的 3 87.87美元 /盎司 ,降到 1 998年 6月份的 2 87.9美元/盎司。由于银需求量增大 ,加之有色金属工业的不景气 ,银产量不仅不能增长 ,而且反而下降。因而人们提出寻找能根据需要而生产的、具有独立开采价值的银矿床 ,即独立银矿床。全世界有三大巨型成矿带 ,我国有四大银成矿区。这些成矿区带的核心是火山 -岩浆活动带。银成矿区带都受巨型或区域深大断裂带控制 ,独立银矿床多产于区域深大断裂带旁侧的次级断层交汇处或附近。独立银矿床的直接围岩可以是火成岩、沉积岩和变质岩 ,但是它们位于火山岩浆活动带中 ,而且以火山岩为主。     

浙江三界、谷来地区1/5万区域地质调查工作的主要进展

三界谷来地区主要出露中、新生代火山岩。进行 １／５万区域地质调查时，采用火山活动旋回－火山构造－火山地层－岩相、岩性－体化思路，按照同旋回火山机构或火山喷发区为单元，确定岩石地层单位和填图单元。火山岩划分为九种岩相类型，建立了两个岩相模式和一个三相一体成因模式。根据火山岩浆作用的旋回性及其产物与火山构造形迹时、空、成因一致性原理，将中、新生代火山岩浆作用分为四个火山活动旋回，圈定了相应的火山机构或火山喷发中心，建立了竹田头复活破火山演化模式。新生代玄武岩中发现二辉斜长麻粒岩等深源包体，为研究区域深部地质作用过程提供了证据。侵入岩按岩石谱系单元划分了七个岩石单元一个超单元，将侵入岩－潜火山岩－火山岩作为岩浆作用整体研究，为正确阐明岩浆作用及其演化规律奠定了基础。区域线型构造发育，与环形火山构造组合，形成火山岩区特有的线一环构造格局。中上元古界陈蔡群变质岩划分为上、下两个岩组，探讨了变质岩的原岩性质及其形成的大地构造环境。     

基于[火用]分析法的矿区工业生态链物质能量流动研究

从工业生态学角度研究矿区工业生态系统的工业代谢和工业生态链，建立矿区物质循环与能量流动[火用]分析和[火用]效率模型。根据生态效率的理念，矿区发展需要五项关键支撑技术，为合理选择煤炭的产业链延伸途径打下理论基础，促进矿区可持续发展。     

Transformation of Organic Matter of the Larch Forest Soils in the Northern Taiga of Nizhne-Tungusskoe Plateau, Central Siberia

The evaluation of biospheric role of the boreal forests in the accumulation of carbon is connected with the evaluation of organic matter (OM) pool in soils. The research sites were larch forests, they are situated on Nizhne-Tungusskoe Plateau. Larch forests of feather-moss and lichen types (110 and 380 years old) were formed on 'ochric podbur' soils. Litter stocks are 3.5–4.5 kg m^{− 2} with thickness 10–25 cm. Cryomezomorphic northern taiga soils contains 38–73 t (carbon) ha^{− 1}. Pool of fast mineralized OM has average value 38.1 t (carbon) ha^{− 1}, including 20.5 and 6.4 t (Carbon) ha^{− 1} of labile compounds on surface and in the soil, and 11.2 t (carbon) ha^{− 1} of mobile OM. Microbial mass reaches 1.78–3.47 t (carbon) ha^{− 1}, its proportion is 3.6–4.9% of the total OM carbon. Zoomass of feather-moss larch forest is 0.20–0.61 * 10^{− 2}, in lichen larch forest −0.01–0.07 * 10^{− 2} t (carbon) ha^{− 1}. A pool of resistant to biological decomposition and bonded to mineral soil matrix OM is 17.7 t (carbon) ha^{− 1} and it varies from 18.6 to 29.0 in feather-moss larch forest, and from 6.4 to 17.0 t (carbon) ha^{− 1} in lichen larch forest. Two-years field experiment has been performed to determine transformation rates of various plant litter fractions and to clarify the role of soil biota in these processes. The results showed participation of all biota groups in the decomposition of plant residues caused weight loss of larch-needles and root mortmass. Isolation of organic matter from all-size invertebrate groups leads to some decrease of decomposition activity.     

车用催化转化器及其对发动机性能影响的研究

本文论述了影响催化转化器性能的主要因素有催化剂，催化剂的中毒失效，催化转化器的结构和排气系统的影响，温度、发动机工作状况等；强调催化转化器的结构与发动机及排气系统匹配的重要性。