广西玉林市东郊区爬行动物的调查研究

从2004年3月至2008年11月对广西玉林市东郊区的爬行动物进行了调查研究,发现该地有爬行动物32种,隶属于3目11科27属．其中优势种有4种,常见种有11种,稀有种有17种．区系成分以华南区的成分占优势,也含有古北一东洋界、华中一华南区成分。与广西其他地区和广东肇庆七星岩地区的爬行动物的相似系数作了比较．     

内马铁路东非大裂谷区地裂缝发育特征及成因分析

地裂缝是一种严重的地质灾害。在建内马铁路途经构造活动现今活跃的东非大裂谷段,铁路施工期间沿线观测到多处地裂缝。为查明研究区地裂缝的发育特征,厘清内马铁路东非大裂谷地裂缝的产生原因,本文通过综合物探技术、钻探和挖探等探测技术,并开展综合勘探地质-地球物理解释,研究结果表明：内马铁路东非大裂谷段地裂缝发育具有切割发育宽度小、深度浅、延伸长度短的特征。钻井和浅层地质-地球物理结构调查显示,内马铁路东非大裂谷段基底以火山凝灰岩熔岩流与裂谷碎屑岩互层组成,埋藏深度为36-50米。通过分析研究区先存和新产生地裂缝的分布发现地裂缝的形成通常与基底正断层共生,表明地裂缝的形成由深部伸展张应力控制;卫星数据显示,新的地裂缝经常暴雨之后发育,并与深部断裂共生,大部分地裂缝终止于压实强度较大的路基附近。表明降水为地裂缝再次活化和扩张的驱动力,而表层地质条件的加固有利于阻碍地裂缝的进一步发展,为研究区地裂缝灾害的防护提供理论支撑     

An virtual numerical experiment to understand the impacts of recovering natural vegetation on the summer climate and environmental conditions in East Asia

By applying a regional integrated environmental model system (RIEMS), a virtual numerical experiment is implemented to study the impacts of recovering natural vegetation on the regional climate and environmental conditions. The results show that recovering the natural vegetation in large scale could have significant influence on summer climate in East Asia. Not only would it be able to change the surface climate, but also to modify to certain extent the intensity of monsoon circulation. Although this is a virtual experiment at an extremely ideal condition, the implication of the simulating results is that the on-going nation-wide activities to recover the crop land for forest and pasture must be managed according to the local natural climate, hydrological and soil conditions. Only under such a condition, would the recovering of natural vegetation bring about significant climate and environmental benefits at regional scale.     

Discovery of Ordovician acritarchs in Buqingshan ophiolite complex, East Kunlun Mountains and its significance

This note reports the first discovery of Middle-Late Ordovician acritarchs from the Buqingshan ophiolite complex of the southern ophiolite zone of East Kunlun. The acritarch assemblage is dominated with acanthomorphids (approx. 32%) and sphaeromorphds (approx. 63%) and contains more characteristic forms, such as Lophosphaeridium edenense, L. varum, Nothooidium sp.,? Buedingiisphaaeridium sp., Visbysphaera sp., Strophomorpha sp., etc. In addition, some tube-like fragments and tetrads, which are recognized as affinity to terrestrial plants and usual occurrence in Late Ordovician-Early Silurian strata, are preserved together with acritarchs. All the known fossil evidence indicates that the strata should be Middle-Late Ordovician in age. It not only provides paleontological proof for the existence of Ordovician ophiolite, but also challenges the usual ideas on strata composition of the studied area and the southern ophiolite zone of East Kunlun, and the models on tectonic framework and evolution of this area and the northern part of the Qinghai-Tibetan Plateau.     

济南市生态保护与建设研究

生态区划是实现区域经济发展与生态环境相协调的基本途径之一,根据济南市的生态环境现状,依据生态区划的原则和方法,建立起适应济南市生态保护与建设区划的指标体系,将济南划分为不同的生态区域,并在分析每个生态区存在的问题的基础上,提出了各区生态保护与建设的措施。     

1995～1999年<暨南大学学报>统计与分析

对１９９５－１９９９年《暨南大学学报（自然科学与医学版）刊载的论文进行统计和分析,根据结果,讨论了论文的学术及其社会效益。     

Relationship between East Asian winter monsoon, warm pool situation and ENSO cycle

Based on the observational data analyses and numerical simulations with the air-sea coupled model (CGCM), a new perspective on the occurrence mechanism of ENSO is advanced in this paper. The continuous strong (weak) East Asian winter monsoon will lead to continuous westerly (easterly) wind anomalies over the equatorial western Pacific region. The anomalous equatorial westerly (easterly) winds can cause eastward propagation of the subsurface ocean temperature anomalies (SOTA) in the warm pool region, the positive (negative) SOTA have been in the warm pool region for quite a long time. The eastward propagating of positive (negative) SOTA along the thermocline will lead to positive (negative) SSTA in the equatorial eastern Pacific and the occurrence of El Niño (La Niña) event. After the occurrence of ENSO, the winter monsoon in East Asia will be weak (strong) due to the influence of El Niño (La Niña).     

巨野煤田含煤地层层序单元划分

运用当代层序地层学的理论和方法体系,通过对区内近２００个钻孔岩心的详细研究,根据石岩－二叠系沉积旋回特点,系统地分析了沉积体系、层序地层及其内部构成特点,建立了研究区陆表海盆地和陆相盆地的层地层格架。研究表明,巨野煤田石岩－二叠系共划分为２个构造层序,７个Ⅲ级层序和４２个准层序。     

跨世纪东海渔业资源利用和管理若干问题的探讨

应用近几年调查研究和监测资料,对世纪之交东海渔业资源的利用现状和存在问题作出了分析和评价,并较系统地分析、阐述了渔业资源开发利用潜力和应采取的相应对策。针对目前东海渔业管理上出现的新情况、新问题,从合理、科学和持续利用东海渔业资源的角度考虑,提出了延长伏季休渔时间、实施拖虾休渔期、规范电脉冲捕捞和管理、完善张网休渔管理、加强梭子蟹资源保护、严格渔具标准、限制作业调整范围等渔业管理方法、措施和建议方案。     

东辽河上下游非点源污染特征对比分析

采用径流分割法估算东辽河下游非点源负荷,对比分析东辽河上下游非点源污染特征,为东辽河水环境治理提供科学依据。结果表明,东辽河下游非点源COD占比为61%~83%,非点源氨氮占比为55%~69%,均高于上游地区;这与同时期农业种植面积紧密相关。东辽河上下游非点源污染负荷年内分布不均,上下游非点源COD负荷与降水量、流量一致,峰值均为7月;与COD不同的是,上游非点源氨氮与降水量、流量一致,峰值7月份;但是下游因玉米种植面积大及8月份追肥的影响,下游非点源氨氮比降水量、流量滞后1月,氨氮峰值为8月份。