文山杨柳井铝土矿矿床成因及找矿标志

铝土矿产于第四系残坡积层中,属堆积型,分布于大塘组及威宁组形成的溶蚀漏斗及洼地中。讨论矿床成因及找矿标志。     

Property rights on genetic resources: economic issues

Biodiversity loss is one of the major international environmental problems. This paper analyses the question of how the use of genetic and biochemical resources in biotechnological industries might affect biodiversity conservation. It is argued that the answer will significantly depend on the concrete regimes of property rights on genetic resources and related biotechnological knowledge. One of the main conclusions derivable from this analysis is that a tightening of intellectual property rights may either aggravate biodiversity loss or strengthen biodiversity conservation, depending on various conditions. This result has interesting parallels to the results of second best theory. Furthermore it sheds new light on the debate regarding the relationship between the WTO Agreement on trade-related aspects of intellectual property rights (TRIPs) and biodiversity loss.     

海权的国际法释义——以《联合国海洋法公约》的相关规定为中心

海权是国家主权的自然延伸,是一种具有权利义务内容的法权;海权是国家在海洋中享有的基本权利,是一种安全权和自卫权;海权还是主权国家的发展权。随着国际海洋新秩序的确立,国际社会应该重新认识和定位海权。我国政府应维护我国的海权,推动我国海洋事业的发展。     

《矿产资源法》生态价值承载研究

《矿产资源法》是改革开放后的产物,更多体现的是矿产资源的经济价值,而对矿产资源的生态价值只做出少许原则性规定。随着市场经济的建立和逐步完善,可持续发展理论、循环经济理论的深化以及经济、社会和科技的发展,《矿产资源法》出现了一些＂不适症＂,其中生态价值的缺失就是一个重要表现。生态文明建设必须建立系统完善的生态文明制度体系,实行最严格的源头保护制度、损害赔偿制度、责任追究制度,从而要求正在修改的《矿产资源法》成为生态价值承载的重要法律,以利于真正实现用制度保护生态环境。     

城市浅水型湖泊底泥释磷的通量估算--以南京玄武湖为例

以南京玄武湖为研究对象,通过静态条件下5℃、10℃、15℃、25℃、35℃玄武湖底泥释磷室内实验计算玄武湖释磷速率,得出底泥释磷速率与上覆水温度的关系,进而算出玄武湖北湖每年磷释放量为0．815 t,东南湖每年磷释放量为 1．013t,西南湖每年磷释放量为0．266t．玄武湖每年底泥释磷总量为2．094 t．根据费克定理,建立了间隙水扩散模型,利用模型计算玄武湖北湖每年磷释放量为0．799 t,东南湖每年磷释放量为0．983 t,西南湖每年磷释放量为0．232 t．玄武湖每年底泥释磷总量为2．014t．在不考虑外源污染的情况下,由底泥磷释放造成的内源污染使玄武湖磷浓度年均维持在 0．101 mg/L,超过湖泊富营养化磷标准,因此,在切断外源污染的情况下应采取措施治理磷的内源污染．     

Local Log-Law-of-the-Wall in Neutrally-Stratified Boundary-Layer Flows

It is well known that in a neutrally-stratified turbulent flow in a deep constant-stress layer above a flat surface,the horizontal mean velocity varies logarithmically with height (the so-called `log-law-of-the-wall').More recently, the same logarithmic law has also been foundin the presence of non-flat surfaces, where it governs thedynamics of the areally-averagedvelocity and involves renormalized effective parameters.Here, we analyze wind profiles over two-dimensional sinusoidal hillsobtained both from numerical simulations performed with a primitiveequation model and from wind-tunnel measurements. We showthat also the local velocity profiles behave to a verygood approximation logarithmically, for a distance from the surface of the order of the maximum hill height almost to the top of the boundary layer. Such alocal log-law-of-the-wall involves effective parameters smoothly depending on theposition along the underlying topography.This dependence looks very similar to the topography itself.     

The role of protected areas and land tenure regimes on forest loss in Bolivia: Accounting for spatial spillovers

The conversion of tropical forests to croplands and grasslands is a major threat to global biodiversity, climate and local livelihoods and ecosystems. The enforcement of protected areas as well as the clarification and strengthening of collective and individual land property rights are key instruments to curb deforestation in the tropics. However, these instruments are territorial and can displace forest loss elsewhere. We investigate the effects of protected areas and various land tenure regimes on deforestation and possible spillover effects in Bolivia, a global tropical deforestation hotspot. We use a spatial Durbin model to assess and compare the direct and indirect effects of protected areas and different land tenure forms on forest loss in Bolivia from 2010 to 2017. We find that protected areas have a strong direct effect on reducing deforestation. Protected areas – which in Bolivia are all based on co-management schemes - also protect forests in adjacent areas, showing an indirect protective spillover effect. Indigenous lands however only have direct forest protection effects. Non-indigenous collective lands and small private lands, which are associated to Andean settlers, as well as non-titled lands, show a strong positive direct effect on deforestation. At the same time, there is some evidence that non-indigenous collective lands also encourage deforestation in adjacent areas, indicating the existence of spillovers. Interestingly, areas with high poverty rate tend to be less affected by deforestation whatever tenure form. Our study stresses the need to assess more systematically the direct and indirect effects of land tenure and of territorial governance instruments on land use changes.