Understanding the synchronisms and anachronisms of the Columbia River Treaty in relation to the principles of international water law

Based on the theory of the politics of international law and the hermeneutic theory for international relations, this paper aims to demonstrate how the history and contextual changes within the Columbia River Basin have affected the underlying principles of the Columbia River Treaty with those of international water law.     

A Power Law Model for River Flow Velocity in Iowa Basins

This study explores power law relationships to estimate water flow velocity as a function of discharge and drainage area across river networks. We test the model using empirical data from 214 United States (U.S.) Geological Survey gauging stations distributed over the state of Iowa in the U.S. The empirical data are the measurements of the mean cross‐sectional velocity and concurrent discharge. The data are used to estimate parameters for a state‐wide model and to test for spatial variability for 15 large river basins contained within the state. Spatial differences among the basins are small but some parameters significantly differ from the state‐wide model. Using individual station data, the authors also explore a simpler power law model that disregards dependence on the drainage area. Overall, the study shows that including drainage area improves the model. Our study provides parameter values that can be directly incorporated into a regional scale routing model, and provides a framework for developing flow velocity models for hydraulically similar rivers in the U.S. and the world.     

论环境刑法效率的角色

环境刑法的效率即环境刑法效率,是在环境刑法目的的范围内,通过环境刑法机制的运行,环境刑法收益与环境刑法成本之间的比例关系对环境刑事法律资源的配置与利用所达到的一种法律状态。在环境刑法法律价值中,环境刑法效率与环境刑法公正是一体的关系。在环境刑法运行中,环境刑法效率具体化为环境形式立法效率、司法效率、行刑效率,对环境刑法的运行发挥着指导、评价作用。在环境刑法变革中,环境刑法的变革过程在效率的视角上是一个不断追求环境刑法效率的过程。     

衡阳近五十年暴雨气候特征和变化规律分析

利用统计分析、Morlet小波分析和墨西哥帽小波诊断方法,对近50n衡阳暴雨的时空变化进行分析,得到其变化规律和周期震荡的突变点,结果表明:衡阳暴雨分布不均,其中南、北部偏多,中部偏少,平均暴雨数为3.0次/n;≥100mm暴雨占暴雨总数的11.0%,特大暴雨较少出现;衡阳局地性暴雨占23.6%,主要以区域性和全市性暴...     

焦化废水中有机物曝气吹脱条件下的挥发特征

焦化废水中各类有机物表现出不同的挥发特征,乙苯、萘等１１种物质比较容易挥发,１２ｈ空曝后其去除率约为２０％￣４０％,它们的挥发速率常数Ｋｖ与Ｈｅｎｒｙ常数间具有良好的线性相关关系,线性相关方程为Ｋｖ＝２．９０６×１０＾３Ｈ＋０．０１４６,挥发作用在这类物质的去除中起着重要作用;苯酚等１２种物质具有中等程度的挥发性;间苯二酚等物质其挥发作用不明显。     

长光路傅立叶变换红外光谱技术研究氯氟烃替代物与氢氧自由基反应速率常数

利用长光路傅立叶变换红外光谱技术（LP－FTIR）,用相对速率方法研究大气中氯氟烃替代物HFC152a（CHF₂CH₃）和HCFC22（CHClF₂）与OH自由基反应速率常数,用紫外光照射O₃和H₂O的方法产生OH自由基。实验测定了700Tor大气压力和常温（298±2k）下的反应速率常数值：k（HFCl52a＋OH）＝（2.90±0.09）×10^－14cm₃·molecule^－1．S^－1,k（HCFC22＋OH）＝（3.80±0.24）×10^－15cm3．Molecule^－1．S^－1,统计误差为2σ     

二甲基硫醚光解及二甲基二硫醚生成速率研究

用低压汞灯照射二甲基硫醚（ＤＭＳ）,在２０ｍ的长光池中用富里叶红外光谱仪测量其光解产物,结果表明二甲基硫醚光解生成二甲基二硫醚（ＤＭＤＳ）和乙烷。测量其不同光照时间的光解产物,结果表明Ｉｎ＾ｃ０／ｃｔ在直解坐标上是一条直线,说明了二甲基二硫醚生成按生一极反应进行,其生成的速率常数为８．７０×１０＾－５ｓ＾－１用低压汞灯照射ＤＭＳ＋Ｈ２Ｏ２体系,富里叶红外光谱检测其产物,在有足够的Ｈ２Ｏ２情况下,生     

一硫代磷酸酯杀虫剂的酶促降解

从降解菌ＹＦ１１中提取了降解权衡利弊并测定了该降解酶对对硫磷,甲基对硫磷和杀螟松的降解特性。对硫磷和甲基对硫磷酶促降解的最适ｐＨ均为８．０,杀螟松的最适ｐＨ为８．５,最适温度为３２．５℃,该降解酶对对硫磷,甲基对硫磷和杀螟松的米氏常数分别为１８７．２,２０５．５和２１２．４ｍｍｏｌ／ｍｌ。     

环境资源保护法适用刑法的思考

新刑法增加破坏环境资源保护罪,标志着我国环境资源保护法制建设的日臻完善,但也给环境资源法如何适用刑法带来一些需要思考的问题。从环境资源法适用刑法的形式,新刑法的特点,环境资源法如何与新刑法接轨等几方面进行了初步探讨,并就环境资源法适用新刑法存在的问题提出几点立法建议。      

Evaluation of trajectories calculated from ecmwf data against constant volume balloon flights during etex

This paper validates trajectories calculated from ECMWF analyses against the tracks of constant volume balloons (CVBs) released during the European tracer experiment (ETEX). The altitudes of the calculated trajectories were adjusted to the altitudes of the respective balloons in short intervals to allow direct comparisons. The agreement between the calculated trajectories and the balloon tracks was very good for the first experiment (individual errors from 1 to 26%, average 15%), and excellent (errors from 2 to 11%, average 6%) for the second one. The agreement for the second experiment was probably partly better because the CVBs travelled above the planetary boundary layer, but the small errors also indicate that the ECMWF fields of the horizontal wind were of exceptionally good quality in the second experiment. This is in sharp contrast to the results of the dispersion models which all failed in the prediction of the perfluorocarbon tracer dispersion for the second experiment. A likely explanation for this is that vertical motions, possibly on small scales, were not correctly captured by the ECMWF analyses, but it is not possible to clarify this with the CVB data.