渤海湾西侧泥质海岸带全新世岸线的变化与海洋的影响

以渤海湾泥质海岸带为例,从形态和地层证据2个方面总结了全新世岸线变化与海洋作用对该地区海岸带发育的影响。中全新世以来千年级别的岸线变迁至少以6次停顿（形成贝壳堤和泥质岭地）和岸进的交替为特征。过去130年间10年级别的岸线变化分为4个阶段,显示了＂小冰期＂结束后随气温上升而发生的岸线自然蚀退是如何逐渐被人类活动（特别是2000年以来的围海造陆）所取代的。全新世海相沉积中发现的9个峰值期和晚全新世的7次风暴驱动事件,表明了研究区泥质海岸带增强的海洋影响。这些结果提供了一条经由地质背景认识现代泥质海岸带过程的途径。     

三峡库区地质灾害防治

通过三峡库区地质灾害现状,规划前期调查和勘察、先期工程治理等方面的阐述,阐明地质灾害治理工作在三峡库区建设中的重要性及其产生的经济效益和社会效益。     

渤海湾西岸风暴潮:叠加地质因素的新探讨

通过对渤海湾西岸1895年以来11次风暴潮高水位的厘定,证实并确定了50年、100年、200年直至10000年一遇的风暴潮高水位值。定量评估了风增水与波浪对风暴潮高水位的贡献。进一步从地学角度讨论了21世纪10年间隔的海面上升量、地面下沉与围海造陆共同作用、海面上升引发的净增水效应及河口增水效应。根据上述各类参数,预测了至2050年的10年间隔、50~10000年不同重现期的极端水位,并讨论了地面下沉对风暴潮测量准确性的影响。认为当前的防潮堤(海垱)高度可抵御50~100年一遇的风暴潮的侵袭,但据所讨论的综合因素的影响,建议2020年防潮堤的高度应达到+4.8m,2030年达到+5.1m(85高程)。     

川东北元坝地区三叠系飞仙关组储层地质模型

依据对川东北元坝地区飞仙关组沉积岩石学特征、储集空间类型及物性分布特征的综合研究,对该地区的储层特征加以抽象和概念化,建立了飞仙关组储层地质模型。地质模型揭示元坝地区海相碳酸盐岩储层段均发育在台地边缘沉积区。其中,台地边缘浅滩最为发育,台地边缘斜坡次之,未见台地边缘生物礁。飞仙关组一段至二段下部为台地边缘斜坡沉积,二段上部至三段为台地边缘浅滩沉积。认为飞仙关组二段和三段的鲕滩沉积储集岩为下一阶段勘探开发的重点,其中飞仙关组二段孔隙—裂缝性储层的勘探开发潜力尤为巨大。     

渤海湾西岸细砂质潮间带的成因分析

根据在海河口南缘至独流减河岸段潮间带地区采集的36个表层和1个无扰动柱状沉积物样品的粒度分析结果,探讨了该岸段的粒度分布特征.结果表明:平面上(自南向北),该潮间带表层沉积物由粉砂质砂变为细砂,呈逐渐变粗、分选性变好的趋势;垂向上,潮间带表层45 cm以下主要为粉砂质砂和粘土质粉砂的互层沉积,向上,渐变为细砂或极细砂,显示向上变粗、分选性变好的趋势.这一向北、向上变粗、分选变好的总趋势,是近半个世纪以来因海河防潮闸的修建而使河流泥砂输运能力降低、近岸海洋影响增强的海河三角洲退化的现代过程的反映.     

应用模糊综合评判原理评价安全煤柱的留设

勘探阶段如何定量评价在厚度较大的新生界下采煤时,如何确定留设安全煤柱的水文工程地质条件,目前尚无完善的方法。以新郑矿区煤田地质勘探获取的水文地质及工程地质资料为例,选取新生界底部含水层、隔水层、风化带、煤层上覆岩组的水文地质及工程地质特征及区域地应力状态五个指标,采用模糊综合评判方法,对矿区留设安全煤柱的水文地质及工程地质条件进行综合评价。评价结果表明:研究区安全煤柱留设条件的优良级得分为48分,中等级得分为33分,较差级得分为19分,表明该矿二1煤层留设安全煤柱的水文地质及工程条件较好。研究结果可为矿区留设安全煤柱提供参考。     

A new ice sheet model validated by remote sensing of the Greenland ice sheet

Accurate prediction of future sea level rise requires models that accurately reproduce and explain the recent observed dramatic ice sheet behaviours. This study presents a new multi-phase, multiple-rheology, scalable and extensible geofluid model of the Greenland ice sheet that shows the credential of successfully reproducing the mass loss rate derived from the Gravity Recovery and Climate Experiment (GRACE), and the microwave remote sensed surface melt area over the past decade. Model simulated early 21st century surface ice flow compares satisfactorily with InSAR measurements. Accurate simulation of the three metrics simultaneously cannot be explained by fortunate model tuning and give us confidence in using this modelling system for projection of the future fate of Greenland Ice Sheet (GrIS). Based on this fully adaptable three dimensional, thermo-mechanically coupled prognostic ice model, we examined the flow sensitivity to granular basal sliding, and further identified that this leads to a positive feedback contributing to enhanced mass loss in a future warming climate. The rheological properties of ice depend sensitively on its temperature, thus we further verified modelâ?s temperature solver against in situ observations. Driven by the NCEP/NCAR reanalysis atmospheric parameters, the ice model simulated GrIS mass loss rate compares favourably with that derived from the GRACE measurements, or about ?147 km³/yr over the 2002–2008 period. Increase of the summer maximum melt area extent (SME) is indicative of expansion of the ablation zone. The modeled SME from year 1979 to 2006 compares well with the cross-polarized gradient ratio method (XPGR) observed melt area in terms of annual variabilities. A high correlation of 0.88 is found between the two time series. In the 30-year model simulation series, the surface melt exhibited large inter-annual and decadal variability, years 2002, 2005 and 2007 being three significant recent melt episodes.     

公路隧道雷电防护研究

通过对太行山区隧道机电设备频遭雷击事件的调研,分析了雷击灾害频发的河北省邢和隧道的地理、气象环境,并对雷击现场进行多次测试研究,对隧道防直击雷和雷电电磁脉冲两方面采取以下5项防雷措施:①建筑物及室外电力设施的直击雷防护,②高压线路的雷电过电压防护,③低压配电及弱电设备的过电压防护,④屏蔽,⑤等电位连结。经过几年的实地验证,防雷措施初见成效。     

An observational and modeling study of a sea fog event over the Yellow Sea on 1 August 2003

A dense sea fog episode that occurred near the coastal city of Qingdao in the Shandong Peninsula of China on 1 August 2003 is investigated by using all of the available observational data and high-resolution modeling results from the Regional Atmospheric Modeling System (RAMS). This fog event reduced the horizontal visibility to be less than 60 m in some locations and caused several traffic accidents locally. In this paper, all of the available observational data, including visible satellite imagery of Geostationary Operational Environmental Satellite (GOES)-9 and MODerate-resolution Imaging Spectroradiometer (MODIS), objectively reanalyzed Final Analysis (FNL) data issued by the National Centers for Environmental Prediction (NCEP), sounding data at the Qingdao and Dalian stations, and the latest 4.4 version of the RAMS model, were employed to study this sea fog case. We begin with the analyses of the environmental conditions of the sea fog event, including the large-scale conditions, the difference between T _2m (air temperature at 2 m altitude) and sea surface temperature (SST), and the atmospheric sounding profiles of the two stations. The characteristics of this sea fog event was documented by using visible satellite imagery of GOES-9 and MODIS. In order to better understand the fog formation mechanism, a high-resolution RAMS model of dimensions 4 km × 4 km was designed, which was initialized and validated by FNL data. A 54-h modeling period that started from 18 UTC 31 July 2003 reproduced the main characteristics of this sea fog event. The simulated lower visibility area agreed well with the sea fog area identified from the satellite imagery. It is shown that advection cooling effect plays a significant role in the fog formation.     

Timing and duration of growth hiatuses in mid Holocene massive Porites corals from the northern South China Sea

Growth hiatuses in massive corals are usually indicative of past ecological or environmental stresses. Among 37 fossil Porites colonies surveyed from the reef flat of Dadonghai fringing reef at Sanya, Hainan Island, northern South China Sea, seven of them were found to show clear evidence of past mortality, representing a population of ～19%. Among these samples, two of them (SYO‐13 and SYO‐28) display clear growth hiatuses reflecting mortality followed by subsequent recruitment, and five others exhibit a well‐preserved mortality surface and no subsequent recruitment. The growth hiatuses were dated using high‐precision thermal ionisation mass spectrometry U‐series techniques. The age results suggest all the dated corals formed and died in the mid Holocene. Multiple dates below the growth hiatuses suggest that SYO‐13 and SYO‐28 died at 6298 ± 11 and 6929 ± 19 a BP (i.e. years before AD 1950), respectively. Multiple dates above the growth hiatuses indicate that growth in SYO‐13 and SYO‐28 resumed at 6257 ± 14 and 6898 ± 20 a BP, respectively. The calculated durations of growth hiatuses are therefore 41 ± 18 a for SYO‐13 and 31 ± 28 a for SYO‐28, respectively, implying growth resumed within decades after the mortality events. U‐series dating of four other samples with dead heads suggests that they died at 6035 ± 53, 6059 ± 23, 6127 ± 22 and 6474 ± 24 a BP, respectively. In addition, using solution inductively coupled plasma mass spectrometry (ICP‐MS), monthly resolution Sr/Ca and Mg/Ca ratios were determined for the annual growth bands below and above the growth hiatuses for three of the dated samples. The Sr/Ca and Mg/Ca profiles indicate that the three corals probably died in different seasons (from spring to autumn), and the mortality appears to be unrelated to anomalous sea surface temperature‐induced bleaching. Copyright © 2010 John Wiley & Sons, Ltd.