征稿启事

<正>《南阳理工学院学报》是由河南省教育厅主管、南阳理工学院主办的综合性学术期刊.创刊于2009年,双月刊,A4开本,本刊分为自然科学版和社会科学版,单月25日出版,国内外公开发行来稿必须为原创性或评述性论文.要具有创新性、学术性和科学性,务须论点明确、文     

基于专利的难溶性含钾岩石生产钾肥技术分析

难溶性含钾岩石的开发和利用对提高我国钾肥产能，保障粮食生产安全有重要意义。该文围绕难溶性含钾岩石生产钾肥技术，通过专利数据库和专利分析系统，统计了本行业相关的专利数据，并对其进行了各种指标的分析，从而揭示了该技术领域中一些非常有价值的情报信息，为科研立项、课题选择、产品攻关、建立知识产权预警制度等提供一定参考。     

PIC系列单片机片内定时器实时时钟的实现

针对直接用单片机片内定时器作实时计时不准问题，本文提出了一种可以获取与秒成整数倍关系的定时器溢出信号的方法，同时克服定量溢出中信号被其它中断暂停所受的计时影响，实验表明，在4MHz晶振下，计时误差可控制在每天14s以下，本方法也适用于一般的单片机，在PIC87系列上的实验结果表明效果很好。     

大功率变频调速系统参数设置问题的研究

GD2000系列有一个强大的软件信息库,为控制、监测和信息查找提供服务.硬件安装,只是基础,参数设置合理才是让设备运转起来的关键.整个系统包括698个参数,下面分类简单加以论述.     

Comparison of Drought-Resistance about Three Wild Rocky-Grasses

In this experiment, using the methods of drought-stress in the pot and PEG simulative drought-stress, three native rocky-slope grasses Pogonatherum panideum（Lam.） Hack, Erioophorum comosum nees and Cynodon dactylon cultivated in the pots were selected as materials to study their drought-resistance by analyzing the indexes such as the leaf area index, the drying roots accumulation, the holding water ability of leaf, the relative conductance of leaf, the soluble protein, chlorophyll. At the same time, by comparing with membership function value of each index, the order of each grass drought-resistance was decided. The results showed that the drought-resistance of Erioophorum comosum nees was stronger than Cynodon dactylon and drought-resistance of Cynodon dactylon was stronger than Pogonatherum panideum （Lam.） Hack. The purpose of the experimental results was to find theoretical foundations for selecting and cultivating native protecting-slope vegetations to adapt to rocky slopes.     

Developmental modes of the Neoproterozoic-Lower Paleozoic marine hydrocarbon source rocks in China

Based on the researches on rock type, the mode of occurrence, diagnostic minerals and creatures, the sedimentary geochemistry and organic facies of Chinese marine source rocks from wells and outcrops, and on the research findings of developmental modes of foreign marine source rock, the authors consider that it is impossible to objectively make clear the formation mechanism of hydrocarbon source rock with high organic matter abundance by either single mode of preservation or high organic matter productivity. According to the Chinese geological features, the formation mechanism of the Neoproterozoic-Lower Paleozoic marine source rock is generalized into four modes, namely, thermal water activity-upwelling flow-anoxic; carbonate gentle slope-upwelling flow; xerothermic climate-brine euxinic milieu; and humid climate-retained euxinic milieu; as the Lower Cambrian undercompensation basin organic facies （the Tarim Basin, South China and southwestern margin of North China）, carbonate gentle lime mud bound organic facies （the Upper Ordovician in Tazhong region of the Tarim Basin and the Lower Silurian in the Upper Yangtze Platform）, the Middle Cambrian evaporation laggon organic facies （the Tarim Basin and the Upper Yangtze Platform）, enclosed undercompensation terrigenous bay organic facies （the Middle-Upper Ordovician in the west of the Tarim Basin, the Lower Silurian Long- maxi Formation in the Upper Yangtze platform）. Chinese marine sedimentations with lower organic matter abundance are generalized into two modes of consumption-dilution mode of open epicontinental sea and depletion-dilution mode of supercompensation basin.     

The controlling factors and distribution prediction of H2S formation in marine carbonate gas reservoir, China

Generally, there are some anhydrites in carbonate reservoir, as H2S is also familiar in carbonate oil and gas reservoirs. Nowadays, natural gas with high H2S concentration is usually considered as TSR origin, so there is close relationship between H2S and anhydrite. On the contrary, some carbonate rocks with anhydrite do not contain H2S. Recently, researches show that H2S is only a necessary condition of H2S formation. The reservoir porosity, sulfate ion content within formation water, reservoir temperature, oil/gas and water interface, hydrocarbon and some elements of reservoir rock have great controlling effects on the TSR occurrence. TSR deoxidizes hydrocarbon into the acidic gas such as H2S and CO2, and the H2S formation is controlled by TSR occurrence, so the relationship among reaction room, the contact chance of sulfate ion and hydrocarbon, the reservoir temperature has great influence on the TSR reaction. H2S has relatively active chemical quality, so it is still controlled by the content of heavy metal ion. Good conditions of TSR reaction and H2S preservation are the prerequisite of H2S distribu- tion prediction. This paper builds a predictive model based on the characteristic of natural gas reservoir with high H2S-bearing. In the porosity reservoir with anhydrite, the formation water is rich in sulfate and poor in heavy metal ion. Oil and gas fill and accumulate in the gas reservoir with good preservation conditions, and they suffered high temperature later, which indicates the profitable area of natural gas with high H2S-bearing.     

下寒武统大林子组溶解蒸发岩系旋回层序及渗流构造成因

《科学通报》第44卷第16期发表了《华北中新元古代及早古生代地震灾变事件及与Rodinia的关系》[1]一文（以下简称《华北》）,涉及辽宁大连下寒武统大林子组的成因问题.我们曾先后于1984～1986,1993～1995和2001年对该组地层进行过详细的旋回层序、微层序和岩石学及微组构成因研究,对大林子组中段溶解蒸发岩系进行了几至几十厘米的超微层单元逐层观测取样,进行室内显微岩石组构和化学组分分析.本文按层序、岩石组构分析和比较     

怎样读懂环境标志

你能读懂环境标志吗?也许你会奇怪,环境标志已问世八年,十环标识在社会上流传数亿个,为什么要提出读懂环境标志的问题呢?原因很简单,在中国环境标志发展的同时,国际标准化组织成立了ISO/TC207环境管理委员会,开展ISO14000系列标准的制定工作。TC207负责制定有关环境标志的ISO14020系列标准,颁布了ISO14020、14021、14024标准,我国于2000年和2001年全部等同转化为国家标准。正处于技术报告阶段的ISO14025标准,则将影响Ⅲ型环境标志走向。所以,我们进入了要读懂环境标志必须读懂国际标准和国家标准的时段。我们在没有国际标准时,借鉴国外经验,建立了中国环境标志制度,现在有了国际标准和国家标准,就必须补上这一课,照标准办事,再凭经验搞环境标志,就会偏离环境标志的国际潮流。