加速闽西奶业发展的可行性分析

通过对龙岩奶制品市场和龙岩发展奶业的基础调查，结合我市区位优势和交通日益发达利于就近融入闽南经济圈的大好形势，对我市发展奶业的可行性进行了分析，并简要提出一些发展措施。     

安徽省芜湖市市区大气SO2污染特征分析

对1993-2002年芜湖市区大气SO2进行了连续10年的观测,结果表明,芜湖市区大气SO2质量浓度10年平均值为0.023 5 mg/m3,由1993年的0.052 mg/m3减少到2002年的0.012 mg/m3,年平均减少率为4%.2000年以来减少速度加快,大气SO2质量浓度日变化总特征是早晨高、午后低,季节变化是冬季、春季高,夏季、秋季低.同时对芜湖市区大气SO2发展趋势作了分析,并提出了防治和减轻污染的建议.     

The Challenging Topics and Future Directions of the Research in Limnology and Watershed Sciences

Based on reviewing the problems in limnology and watershed sciences in meeting the national demands and the development of theories and methodology, this paper proposed some challenging topics to the sciences, covering the process of lake evolution and the quantitative analysis of human impacts, in -lake nutrient cycling an biogeo-chemical process, the process and mechanisms of material flow in lake-watershed system, digital watershed and the modeling of the surface process of lake -watershed, and ecosystem health and scientific management of lake-watershed.     

湖泊扇三角洲的重要特性

湖泊扇三角洲作为重要的油气储集体广泛分布于我国东部含油盆地中，文章在分析湖泊扇三角洲形成条件的基础上，指出扇三角洲发育前缘席状砂，阐述了湖泊三角洲的岩性，结构，沉积构造以及地球物理特性，建立了区域性沉积模式，研究表明，前缘席状砂是良好地油气勘探目标。     

东平湖轮虫群落与水质评价

报道了东平湖轮虫群落结构特征及数量的季节变动,并依据调查结果,采用“指示生物法”“生物指数法”和“Ｒ．Ｍａｒｇａｌｅｆ多样性指数法”评价该糊水质状况及营养化程度,研究表明,轮虫对水体污染具有较好的指示作用,东平湖水质属于寡污－β中污至β中污型,且各采样站水质污染程度有的差别。     

山丹湖环境水化学特征的主因子分析

用因子分析法和相关的统计方法研究了山丹湖的富营养化特征,从原始数据的相关矩阵出发,提取了占总方差８２％的两个主因子,并对主因子作出合理的解释,主因子分析的结果表明,由氮营养化引起的污染是控制山丹湖营养化学特征的主要因子。     

Holocene lake deposits of Bosten Lake, southern Xinjiang, China

A 9.25-m-long sediment core from Bosten Lake,Xinjiang, provides detailed information about changes in the water budget and biological acticity over the last 8400 cal-endar years. The chronology is constructed from six AMS radiocarbon dates on the terrestrial plant remains. Based onanalyses of TOC, CO3, detrital compounds and biogenic SiO2,lake level fluctuations and periods of remarkably-negative water budget appeared at 8.4-8.2 cal ka, 7.38-7.25 cal ka,5.7-5.5 cal ka, 3.7-3.4 cal ka and 3.3-2.9 cal ka, respec-tively. As they are in-phase with low lake levels at Sumxl Co and Bangong Co in western Tibet Plateau and with paleo-lakes in Inner Mongolia, a climate-induced change to some-what drier and warmer conditions is inferred. A further drop in lake level after 1320 AD of about 200 yr duration may heattributed to a negative water balance prior to the main phase of the Little Ice Age. Deep and stable lake phases of 1500 yr and 1800 yr duration at 7.2-5.7 cal ka and 5.5-3.7cal ka coincide with maximum moisture during the Holocene Megathermai in China. The long term trend towards aridity since about 4.3 cal ka can dearly be recognised. The reduced water budget of Bosten Lake from 640-1200 AD may be attributed to local effects.     

Temperature variations on the Tibetan Plateau over the last two millennia

The paleoclimate data recovered from ice cores,tree rings and lake sediments indicate regional features of cfimatic change on the Tibeta n Plateau (TP) during the last 2000 years. The composite temperature reconstructions in-dicate that several main climatic episodes, such as the “LittleIce Age“ between 1400 and 1900, the “Medieval Warm Pe-riod“ in 1150-1400, a less warm period in 800-1100, and an earlier cold period between the 3rd and 5th centuries,occurred in the TP. In addition, temperature varied from region to region. The period from AD 800 to 1100, which waswarm in northeastern TP, was contemporaneous with cool-ing in the western and southern TP. The southern TP ex-perienced warming between 1150 and 1400. For western TP,the δ^18O records of the Guliya ice core indicate that the pe-Hod 1250-1500 witnessed a clear warming. Large-scaletrends in the temperature history from northeastern TP aremore similar to those in eastern China than are the trendsfrom the Guliya ice cap far to the west and southern TP. The most prominent similarities between the temperature varia-tions of the TP and eastern China are such cold phases as 1100-1150, 1500-1550, 1650-1700 and 1800-1850, andthe latter three cold events match with three widespreadg lacial advances which occurred on the TP during the Little Ice A2e.     

110kV GIS市区变电站设计技术

ll0kV市区变电站设计是城网建设中较为关键的技术环节。根据无人值班变电站要求，提出l10kV市区变电站应从电力系统整体出发。力求电气主接线简化，配置与电网结构相应的保护系统。简化电气主接线，提高可靠性，电气设备的质量和技术特性极为关键。由于科学技术的进步，现在已发展为全封闭组合电器(GlS)。同时，市区变电站必须坚持节约用地、减少建筑面积的原则，及随着城市居民对居住环境的要求日益提高，ll0kV市区变电站宜采用全户内布置方式。