富砂地层格架高分辨率层序地层学研究及储层甜点预测——以四川盆地合川地区须家河组为例

富砂致密砂岩储层的甜点预测是领域研究的一个关键和难点,以四川盆地中部合川地区须家河组二段为例,探索从继承性古地貌控制下的高分辨率层序地层学角度来展开研究。基于须二段沉积前雷口坡组岩溶古地貌恢复,认为继承性发展的岩溶古地貌控制了须二期地层的沉积充填,建立了须二段砂体向周缘地貌高地渐次超覆的地层充填模式。以该模式及高分辨率层序地层学理论为指导,综合利用地震、测井、岩芯等资料,在识别不同级别层序界面和湖泛面类型的基础上,将须二段划分为1个长期基准面旋回,又包括6个中期基准面旋回,自下至上为MSC1-MSC6。其中,MSC1-MSC3整体发育退积式辫状河三角洲,向南东超覆,属于上升半旋回;至MSC4达到最大湖泛面之后,随即进入下降半旋回;MSC4-MSC6发育进积式辫状河三角洲,粒度逐渐向上变粗。以基础资料最为丰富的MSC3为例,在层序格架内建立了“古地貌-层序厚度-砂体厚度-砂体物性-甜点分布”的相关关系,预测了有利储层甜点分布区。这些研究思路方法可供富砂致密砂岩储层研究,特别是井网稀疏、地震资料丰富但分辨率有限的地区研究参考,具体认识可直接应用于区域油气勘探部署。     

安徽省地质灾害隐患点现状分析与研究

基于2015年安徽省地质灾害统计数据,对全省地质灾害隐患点的类型、数量、规模等进行了汇总与分析;总结了地质灾害隐患点的时空分布规律,初步探讨了灾害形成的原因;根据地质灾害隐患点评价指标体系,划分了安徽省地质灾害隐患点等级;提出了地质灾害防治工作方向与措施建议。     

PROGNOSIS OF AGGRADATION IN THE LOWER YELLOW RIVER BY HISTORIC ANALYSIS OF THE MORPHOLOGY OF ITS ABANDONED ANCIENT CHANNEL

1. INTROOUCnONFor a long time, the Lower Yellow River has been aggtading. As a result, the river bed becomesmuch higher than the adjacent land beyond the levees and poses a threat to the safety of the GreatNorthern Plain of China. Since the founding of the New China, great success has been achieved insafeguarding the levee for forty years. The trend of aggravation in lower reaches however is still Soingon and is at a rate even higher than before. That makes the flood control on the LO…     

中国大城市拆迁安置居民补偿方式与受益率测度 ——以南京为例

拆迁安置补偿是城市内城改造与扩张过程中涉及拆迁居民利益的核心问题,拆迁安置家庭多个特征因影响补偿方式和受益率。针对补偿方式不同与受益率不同,分别采用二项逻辑回归与多元线性回归模型,对南京市4个安置区的349户拆迁安置居民家庭进行了实证分析,结果表明：① 对于实物补偿和货币补偿,城中村拆迁安置居民家庭和夫妻双方职业均为“无业”的家庭更容易获得实物补偿。② 单从经济角度来讲,城中村拆迁安置家庭成为拆迁安置家庭中的最大受益者,7人及以上的大家庭、高学历家庭也是货币补偿中的受益者。但其受益并非是由市场化的结果造成,而是市场作用与计划经济旧有制度的共同使然。因此,建立公平合理的补偿机制是解决问题的关键。     

Determination of PCB-contaminated sites in Belarus： A case study

PCBs belong to POPs of priority concern in Belarus due to the large amount of PCBs, long period of PCB and PCB-containing equipment usage and possibilities of PCBs dissemination in the environment. From the point of health risk assessment the revealing of PCBs contaminated sites is very important. The greatest amounts of PCBs in Belarus are used in electrical equipment; therefore experimental work was conducted on the territories where PCB-containing electrical equipment is installed or stored. About 20 sub-stations with capacitors and 2 places with transformers were investigated. More than 200 soil and bottom sediments were collected and analyzed. 6 individual PCBs congeners （PCB-28, PCB-52, PCB-138, PCB-153, PCB-180 and PCB-203） were detected by gas chromatography and chromatography mass spectrometry. PCBs contents in the soils of the territories, where electrical equipment is used and stored, come up to milligrams or sometime grams per kilogram. Maximum concentrations of PCBs （2-21 g/kg） were tracked in the soil near destroyed capacitors and transformers as a consequence of PCB leakage. The highest concentrations of PCBs are found in topsoil layer. In some cases high PCB concentrations are fixed at the depth of 50 cm. In several cases PCB leakage can be easily noticed due to dark color. Low chlorinated PCBs prevail in the soils of the places where capacitors are installed or stored, and high chlorinated PCBs are noticed where transformers are stored. As a rule, contaminated areas are rather local （typical spot is less than a square meter）. Nevertheless, they are potentially sources of secondary ground and surface water, as well as bottom sediments pollution. Moreover, spreading of PCBs beyond the places of PCB-containing equipment usage or storage occurs： the sum of 6 PCBs at the distance of 100-150 m from capacitor battery comes up to 0.35-4.6 mg/kg in the soil. Soils at practically all investigated sub-stations are polluted with PCBs. In most cases high concentrations of PCBs are revealed. On the whole, spatial structure of PCB contamination soil is extremely heterogeneous.     

基于CMIP6的中国未来高温危险性变化评估

评估高温灾害的危险性变化,能够为区域高温灾害风险管理和制定减灾措施提供决策依据。本研究选取高温日数、最高温度和平均高温强度3个指标,基于1961—2020年中国2517个气象站点日最高温数据和CMIP6情景模式比较计划中SSP2-4.5情景下12个气候模式提供的2031—2099年未来气候预测数据集,用核密度概率估计方法计算了4个重现期（即5、10、20和50年）下3个指标的取值,对中国未来高温危险性变化进行了评估。结果表明：① 在SSP2.4-5情景下,中国的高温日数呈现出4个危险中心,分别是：西北干旱（半干旱）地区中部、华北和华中地区的交汇区域、西南地区中部和华南地区南部,并且高温日数从这4个中心向外逐渐减少;最高温度在空间上的分布北部大于南部,东部大于西部。平均高温强度的分布则呈现出从华北地区南部、西北干旱（半干旱）地区西部和东部地区西部向我国除青藏高原地区外的其它地区减少的趋势; ② 在SSP2.4-5情景下,随着重现期年限的增长,中国地区3个高温指标均呈增长趋势且增幅较大,并且高值范围也在不断扩大;③ 3个高温指标变化值均呈现出了明显的空间聚集性,3个指标共同显示的热点区域包括西南地区北部和南部、西北干旱（半干旱）地区中部和华北、华中地区的少部分区域,这些地区发生高温灾害的可能最大,同时根据高温日数变化和最高温度变化,东部地区西部发生高温灾害可能也较大,3个指标共同显示的冷点区域包括青藏高原地区东南部、西北干旱（半干旱）地区的西部和我国东南沿海地区,这些地区几乎不会发生高温危险。     

三维AVO分析及在黄骅坳陷港186井区的应用

利用Hampson-Russell／Geoview／AVO软件研究含气砂岩的地震反射振幅随炮检距的变化关系及AVO属性的特征。并将AVO技术应用于大港油田黄骅坳陷港186井区的天然气藏研究。结果表明,在地质条件复杂的地区,三维AVO分析可区分真假天然气响应,准确确定已知气藏及异常区的空间展布范围。     

对虾白斑杆状病毒(WSBV)对斑节对虾的实验感染与病理学研究

用取自发病虾塘患典型白斑病的病虾为毒源 ,对健康斑节对虾Penaeusmonodon进行人工感染 ,按Koch氏法证实了对虾白斑杆状病毒 (WSBV)是白斑病的病原。对人工感染WSBV后患典型白斑病的斑节对虾的胃、肠及皮下结缔组织进行石蜡切片和超薄切片 ,研究WSBV引起的组织病理变化和宿主细胞感染WSBV后的超微病变过程。结果表明 :感染WSBV后病虾的不同组织均存在广泛的变性、坏死 ,上皮细胞大量解体、脱落 ;部分细胞核肿大、游离 ;结缔组织糜烂 ,呈现空泡化 ;未发现包涵体。透射电镜照片显示 :感染WSBV后的病虾在感染前期 ,靶细胞核膨胀 ,核仁消失 ,核外膜破损 ,染色质靠边分布 ,内质网断裂 ,核糖体脱落 ,线粒体肿胀 ,高尔基体萎缩 ,溶酶体空泡化 ;感染中期 ,病毒粒子在细胞核内大量复制 ,直至充满整个核 ,细胞核内无结构化 ,核膜及质膜皱缩 ;感染后期 ,核胀破 ,病毒粒子从核内释放 ,细胞核呈空囊状 ,胞质内髓样结构明显 ,细胞器解体 ,细胞功能丧失。     

核酸探针原位杂交检测白斑综合症病毒的组织特异性

从白斑综合症病毒 (whitespotsyndromevirus ,简称WSSV)部分基因组文库中得到核酸探针 ,采用原位杂交检测方法检测对虾甲壳下表皮、胃、后肠、鳃、触角腺的上皮细胞、淋巴器官的基质细胞、肌细胞、心肌细胞及结缔组织细胞 ,原位杂交结果均为阳性。对虾甲壳下表皮的上皮细胞、胃的上皮细胞对病毒较其它部位敏感 ,感染程度高 ;中肠上皮细胞、肝胰腺上皮细胞、淋巴器官内皮细胞未发现感染病毒 ,原位杂交用于WSSV检测 ,比组织切片HE染色更准确、更敏感。在同一组织的同一部位 ,原位杂交所得到的阳性细胞个数比HE多。探针大小不同 ,敏感性也有变化。短的探针 41 3bp敏感性较高 ,长的探针敏感性降低。     

SIMULATION OF STRONG GROUND MOTION IN AKETAO M6.7 EARTHQUAKE USING THEORETICAL GREEN'S FUNCTION

Aketao M6.7 earthquake on November 25, 2016 occurred in Aketao Country, Kizilsu Kirghiz Autonomous Prefecture, Xinjiang Autonomous Region. In this paper, according to the focal mechanism solution, the geometrical parameters of the fault are used as input to simulate the acceleration records of the surrounding area of Aketao M6.7 earthquake on November 25, 2016 with the QSGRN/QSCMP program. The peak ground acceleration distribution is plotted by extracted peak ground accelerations and site condition correction. Comparison is carried out between the observed waveforms and the simulated waveforms in the time domain and the frequency domain of two strong motion stations. It is verified that the amplitudes of simulated and observed data are equal in magnitude, their calculated residuals are smaller in low frequency range and the spectral characteristics of simulated and observed data are consistent. Furthermore, the simulated peak ground acceleration corresponding to the coordinates of the actual survey points is extracted and compared with the survey spot intensity, and both have good correspondence. This paper attempts to provide a method for rapid output of peak ground acceleration distribution after an earthquake, so as to provide a method for estimating the seismic impact field in areas where the monitoring station is scarce, the topography is complex or it is difficult to implement the rapid earthquake disaster investigation. And it also provides supporting information for rapid assessment of earthquake disaster and emergency decision-making.