首台秸秆混燃发电机组投产 年节约近八万吨原煤

2005年12月16日．我国首台煤粉秸秆混燃发电机组在山东枣庄华电国际十里泉发电厂成功投产。国家发改委有关负责人认为，以秸秆代替煤炭作为发电新能源．是我国生物质能发电领域的重要突破．是利用可再生资源、大力发展循环经济的重要尝试，有利于经济增长方式的转变。作为国内第一个在老机组改造的生物质能发电项目．此项目具有前瞻性、推广性。     

曹松诗歌意象研究

唐代诗人曹松创作甚丰,留给后人一百多首诗歌。在这些诗歌中,诗人经常运用云月意象来表达自己常年漂泊、沦落他乡的凄苦的心境,又运用鹤泉意象营造清幽的环境来慰藉自己。通过对曹松诗歌意象的研究,我们可以充分挖掘出这个封建时代的士子一生凄苦矛盾的心境,这对诗人的研究无疑是有巨大帮助的。     

夏县祁家河乡七泉村滑坡稳定性与防治措施

通过对七泉村滑坡的工程地质勘察,从定性和定量两方面分析了滑坡天然工况下的稳定性,对滑坡提出了相应的防治措施。     

基于SPSS的岩溶地下水质变化及其影响因素——以重庆市金佛山表层岩溶地下水为例

重庆金佛山地区岩溶泉水遍布,但是各个泉点的水质却有较大差异.利用地下水的化学性质,如pH,电导率Υ,HCO-3、Ca2+、Mg2+、Na+、K+、SO42-、NO-3和Cl-等的质量浓度进行因子分析可以分辨出自然过程和人类因素对地下水的影响.2009年1月在重庆金佛山地区采集36个岩溶泉水样,分析结果表明:金佛山岩溶泉的水化学成分具有较大的空间变异.利用SPSS中因子分析方法,得到基于水中离子和地球化学过程解释的地下水水质特征及其形成的4个因子:水-岩作用是地下水中SO42-、F-、K+、Sr2+和Ca2+形成的共同因素,Mg2、HCO3-主要受土壤等因子影响,Na+、Cl-主要来源于大气降水,人类活动主要影响水中的NO-3.以上4种因子可以解释金佛山岩溶地下水水质形成的87.58％,其中水-岩作用可以解释55.56％,是影响金佛山地区岩溶水水质的最重要因素.     

山西辛安泉泉域大型藻类植物分布特点的研究

对山西省辛安泉泉域大型藻类植物的分布特点进行了调查研究.研究结果表明:泉域内大型藻类植物种类丰富,共有55种,隶属于6个门,分别为蓝藻门、红藻门、黄藻门、硅藻门、绿藻门、轮藻门;群落类型多样,共有6大类型,分别为刚毛藻群落、轮藻群落、水绵-双星藻群落、等片藻-直链藻群落、无隔藻群落和串珠藻群落;藻体形态多样,有5种,分别为垫状、胶团状、胶质丝状体、丝状体和簇状;生长季节多样,种类数大致为春季>秋季>冬季>夏季;生境多样,共有4种固着基质,分别为石头、枯木、泥沙和其它藻体.相似性分析结果显示:辛安泉泉域的大型藻类与其它地区的相似指数都很低,一定程度上反映了地域性差异和生殖隔离现象.     

三个泉倒虹吸管管材的选择

结合三个泉工程实际情况，通过对目前大型输水工程几种常用管材的参数、管径、性能及经济效益的比较，用加权法对管材进行综合评价，选择预应力钢筒混凝土管作为三个泉倒虹吸管工程的管材。     

Formation mechanisms of megadunes and lakes in the Badain Jaran Desert, Inner Mongolia

Field observations demonstrate that calc-sinters occurred in the lakes of Badain Jaran Desert. 87Sr/86Sr ratios,14C,δ 13C and mineral com-positions of calc-sinters,and 3He/4He,4He/20Ne,δ 18O,δ D,pH and TDS of water from springs and lakes are analyzed in detail. The results indicate that the lake water is supplied through deep fault zone. The “ker-nel” of stabilized dunes in the Badain Jaran Desert perhaps consists of calc-sinters and calcareous ce-mentation layers. Deep-seated groundwater effuses from this “kernel” and recharges to lakes in desert. Precipitation and snowmelt water from the Qing-hai-Tibet Plateau is fed into the Badain Jaran Desert,Gurinai,Wentougaole and Ejinqi areas through the Xigaze-Langshan Fault zone. The isotopic composi-tions of groundwater in the Alax Plateau are abnor-mal due to the strong evaporation of the Gyaring and Ngoring lake water in the headstream of the Yellow River. Groundwater dissolves dissoluble fractions of rocks during its transportation through the fault zone and flows out of the mouth of spring in the Badan Jaran Desert. The dissoluble fractions are finally de-veloped into calc-sinters and calcareous cementation layers around the spring. Calci-sinters are gradually largened and eventually emerge on the surface of lake water. Eolian sands accumulate on the surfaces of calc-sinters and calcareous cementation layers,and eventually develop into dunes. Invasion of magma causes an increase in the temperature of groundwater within the faults. Groundwater evapora-tion provides water vapor for the formation of humid stabilized dunes during its upwelling. Rhizoconcre-tions found in Yihejigede indicate that the dune was formed and remained immovable 4700 years ago. The height of the megadunes is proportional to thermal quantity carried by the groundwater.