论民国时期河南灾荒的社会成因

民国年间河南灾荒现象异常突出，虽与当时整体气候背景及河南特殊的地理特征相关，但灾荒背后的社会原因更应引起我们的关注。其主要表现为：一、社会经济乏力，百姓抗灾能力低；二、政治腐败，体现在政府的赋税名目繁多、政府官员失职渎职以及挪用、贪污河防公款等几个方面；三、战争与灾荒；四、帝国主义列强对中国的残酷掠夺。     

美国环保超级基金制度的实施及问题

对美国环保超级基金制度作了简要的介绍,指出了其实施过程中的成功与不足,以期为我国环境法制的完善提供有益的借鉴.     

跨界原生质体融合工程菌株改进合成制药废水生物处理的有效性研究

用常规生物法处理合成制药废水难以去除持久性有机污染物POPs，且存在不能稳定达标的问题，应通过用跨界原生质体融合技术，构建出具有高降解性、高絮凝性、高适应性的基因工程菌株来解决上述问题。为检验基因工程茵的有效性，对基因工程茵进行了抗生素遗传性能鉴定和电子显微镜(SEM)的形态鉴定，并在制药废水的污水处理厂进行了基因工程茵的培养和接种。结果表明：基因工程菌株能成功取代原有土著茵并具有显著的优点。     

Experimental study on Cr(Ⅵ) reduction by Pseudomonas aeruginosa

Investigation on Cr( Ⅵ ) reduction was conducted using Pseudomonas aeruginosa. The study demonstrated that the Cr(Ⅵ) canbe effectively reduced to Cr( Ⅲ ) by Pseudomonas aeruginosa. The effects of the factors affecting Cr( Ⅵ ) reduction rate including carbon source type, pH, initial Cr(Ⅵ) concentration and amount of calls inoculum were thoroughly studied. Malate was found to yield maximum biotransformation, followed by succinate and glucose, with the reduction rate of 60.86%, 43. 76% and 28.86% respectively. The optimum pH for Cr( Ⅵ ) reduction was ?.0, with reduction efficiency of 61.71 % being achieved. With the increase of initial Cr(Ⅵ) concentration,the rate of Cr(Ⅵ) reduction decreased. The reduction was inhibited strongly when the initial Cr(Ⅵ) concentration increased to 157 mg/L. As the amount of cells inoculum increased, the rate of Cr( Ⅵ ) reduction also increased. The mechanism of Cr( Ⅵ ) reduction and final products were also analysed. The results suggested that the soluble enzymes appear to be responsible for Cr (Ⅵ) reduction by Pseudomonas aeruginosa, and the reduced Cr( Ⅲ ) was not precipitated in the form of Cr(OH)3.     

Climate impact from peat utilisation in Sweden

The climate impact from the useof peat for energy production in Sweden hasbeen evaluated in terms of contribution toatmospheric radiative forcing. This wasdone by attempting to answer the question`What will be the climate impact if onewould use 1 m<sup>2</sup> of mire for peatextraction during 20 years?'. Two differentmethods of after-treatment were studied:afforestation and restoration of wetland.The climate impact from a peatland –wetland scenario and a peatland –forestation – bioenergy scenario wascompared to the climate impact from coal,natural gas and forest residues.Sensitivity analyses were performed toevaluate which parameters that areimportant to take into consideration inorder to minimize the climate impact frompeat utilisation. In a `multiple generationscenario' we investigate the climate impactif 1 Mega Joule (MJ) of energy is produced every yearfor 300 years from peat compared to otherenergy sources.The main conclusions from the study are:?The accumulated radiative forcing from the peatland – forestation – bioenergy scenario over a long time perspective (300 years) is estimated to be 1.35 mJ/m²/m² extraction area assuming a medium-high forest growth rate and medium original methane emissions from the virgin mire. This is below the corresponding values for coal 3.13 mJ/ m²/ m² extraction area and natural gas, 1.71 mJ/ m²/ m² extraction area, but higher than the value for forest residues, 0.42 mJ/ m²/ m² extraction area. A `best-best-case' scenario, i.e. with high forest growth rate combined with high `avoided' methane (CH₄) emissions, will generate accumulated radiative forcing comparable to using forest residues for energy production. A `worst-worst-case' scenario, with low growth rate and low `avoided' CH₄ emissions, will generate radiative forcing somewhere in between natural gas and coal.?The accumulated radiative forcing from the peatland – wetland scenario over a 300-year perspective is estimated to be 0.73 –1.80 mJ/ m²/ m² extraction area depending on the assumed carbon (C) uptake rates for the wetland and assuming a medium-high methane emissions from a restored wetland. The corresponding values for coal is 1.88 mJ/ m²/ m² extraction area, for natural gas 1.06 mJ/ m²/ m² extraction area and for forest residues 0.10 mJ/ m²/ m² extraction area. A `best-best-case' scenario (i.e. with high carbon dioxide CO<sub>2</sub>-uptake combined with high `avoided' CH₄ emissions and low methane emissions from the restored wetland) will generate accumulated radiative forcing that decreases and reaches zero after 240 years. A `worst-worst-case' (i.e. with low CO<sub>2</sub>-uptake combined with low `avoided' CH₄ emissions and high methane emissions from the restored wetland) will generate radiative forcing higher than coal over the entire time period.?The accumulated radiative forcing in the `multiple generations' – scenarios over a 300-year perspective producing 1 MJ/year is estimated to be 0.089 mJ/ m<sup>2</sup> for the scenario `Peat forestation – bioenergy', 0.097 mJ/ m² for the scenario `Peat wetland with high CO<sub>2</sub>-uptake' and 0.140 mJ/ m<sup>2</sup> for the scenario `Peat wetland with low CO₂-uptake'. Corresponding values for coal is 0.160 mJ/ m², for natural gas 0.083 mJ/ m² and for forest residues 0.015 mJ/ m². Using a longer time perspective than 300 years will result in lower accumulated radiative forcing from the scenario `Peat wetland with high CO₂-uptake'. This is due to the negative instantaneous forcing that occurs after 200 years for each added generation.?It is important to consider CH₄ emissions from the virgin mire when choosing mires for utilization. Low original methane emissions give significantly higher total climate impact than high original emissions do.?Afforestation on areas previously used for peat extraction should be performed in a way that gives a high forest growth rate, both for the extraction area and the surrounding area. A high forest growth rate gives lower climate impact than a low forest growth rate.?There are great uncertainties related to the data used for emissions and uptake of greenhouse gases in restored wetlands. The mechanisms affecting these emissions and uptake should be studied further.     

浅议促进企业进行环境管理的方法

企业是环境污染的重要源头，企业污染是政府进行环境监督、管理的工作重点。但政府单纯凭借法律、行政和经济手段是不够的，还应该充分调动企业自身进行环境管理、参与环境保护的积极性和主动性，即压力和动力并重。为此，政府应加大对社会、对企业的环保宣传力度，使企业认识到环境效益、社会效益和经济效益存在着一致性和互促性。此外，政府还应加在ISO14000环境管理系列标准的宣传，使企业提早准备、积极行动以提高企业在市场中的竞争力。     

秦岭若干重要类型金矿床(体)快速定位预测

本文以西部秦岭地区八卦庙、双王、煎茶岭 3种重要类型金矿床为例 ,在成矿地质背景研究基础上 ,开展若干新方法新技术的找矿试验 ,研究发现 ,八卦庙式金矿岩石的烃含量与其金品位大致成正相关关系 ;而且金矿化强度和规模越大 ,相关系数值也越大 ;据此根据石英脉的烃含量对隐伏金矿床 (体 )和金矿化规模进行预测。双王式金矿原生晕的前缘晕元素为B、As、Sb、Hg,近矿晕元素为Au、Ba(-) ,尾晕元素为Mn、Bi。通过原生叠加晕垂向研究预测 ,双王和八卦庙金矿床现有的金矿体向下延伸还较大 ,在矿床的深部存在有盲矿体。煎茶岭式金矿的矿石铅同位素平均值比围岩要小 ,铅同位素曲线的低峰区往往就指示矿体所在 ;预测区的2 0 6Pb/ 2 0 4 Pb、2 0 8Pb/ 2 0 4 Pb比值变差椭圆图的形状和轴向斜率与已知矿区趋于一致 ,并且两者的变差椭圆图形大部分重叠 ,说明存在有同类型金矿体。以上研究成果为同期或后来的勘探工作或矿山采矿所验证。     

“成型-烧结”碎磷矿的黄磷生产工业性试验

将中小黄磷企业长期堆存的碎磷矿 (粒径 <5mm) ,经过“粘接成型 烧结”及理化指标检测后 ,按烧结矿∶块矿 =1∶1入炉进行工业性试验 ,试验表明该烧结矿可用于黄磷电炉生产 ,该法是降低黄磷生产成本 ,减少环境污染 ,使资源得到合理利用的有效途径之一