珠江三角洲晚第四纪地层、海平面变化 与构造运动的关系

在回顾南海北部海岸和陆架地层证据的基础上,梳理了珠江三角洲晚第四纪演变历史。结果显示：1）本区晚第四纪地层拥有2套海相沉积,上（新）海相层是当前间冰期（或10.5 ka B.P.以来）高海平面期间形成的沉积物,而下（老）海相层最可能是末次间冰期（126―120 ka B.P.）高海平面阶段留下的沉积物;2）老海相层顶面埋深在三角洲盆地内至少比现今海平面低10~15 m,在珠江口一带则低于20 m,这说明珠江三角洲盆地存在构造沉降,因为2次间冰期的海平面高度是相近的;3）在新生代欧亚板块大陆向东南伸展的构造格局下,南海北部陆架和海岸带经历长期连续的沉降,而长期平均沉降率在0.12 mm/a左右,明显低于GPS测出的现代沉降率;4）在这种板块运动基础上,晚第四纪断裂活动增强了三角洲盆地的沉降,为2次海侵提供了可容沉积空间。     

Latest progress on interactions between VLF/ELF waves and energetic electrons in the inner magnetosphere

Interactions between very/extremely low frequency (VLF/ELF) waves and energetic electrons play a fundamental role in dynamics occurring in the inner magnetosphere. Here, we briefly discuss global properties of VLF/ELF waves, along with the variability of the electron radiation belts associated with wave-particle interactions and radial diffusion. We provide cases of electron loss and acceleration as a result of wave-particle interactions primarily due to such waves, and particularly some preliminary results...     

区域主体功能区规划模型、方法和应用研究——以京津地区为例

通过分析国家"十一五"规划中关于区域主体功能区划分的原则要求,将关键自然资本不能减少的强可持续发展生态阈值理论与区域综合生态价值观相结合,受经典力学定律启发,构建了区域主体功能区规划的"承载力-潜力-压力-阻力"模型,提出了计算区域空间开发所受合力的方法,得到了区域主体功能区的综合划分指数,根据规划空间单元综合划分指数的大小实现4类主体功能区地划分,解决了目前区域主体功能区规划中的开发类和保护类的阈值确定这一技术难点。以京津地区为实证,根据对未来发展决策导向的预期,应用区域主体功能区规划模型和方法实现了京津地区4类主体功能区地划分,获得了良好的应用效果。     

加强农村供水建设促进水资源可持续利用

建设农村供水工程,配置恒压变频设备,实行一户一表、以量计征的管理办法是降低耗能和取水成本,提高供水标准,增强群众节水意识的有效措施.介绍了沧州市农村供水现状及存在问题,提出了解决措施.     

山西宁武地区1686年以来年降水重建*

根据山西北部宁武地区的树轮宽度指标,建立了该地区过去318年的树轮STD,RES和ARS年表,发现上年8月至当年7月 (全年)的降水与差值年表(RES)显著相关 (r=0.71, n=50),在此基础上设计了转换方程,重建了宁武地区1686年以来的全年降水,方差解释量达到 48.6％(调整自由度后为46.8％, r=0.697,F=26.471, p<0.0001)。降水量较少的时段为1693~1710年,1720~1764年,1825~1841年,1873~1882年,1901~1930年,1966~1972年和1988~2003年,降水量较多的时段为1711~1720年, 1765~1824年,1842~1872年,1883~1886年和1931~1987年。 历史文献记录的干旱年份在重建序列上均有所反映。重建序列与贺兰山1~7月降水显著相关 (99％置信度下, r=0.312)。功率谱分析表明山西宁武上年8月至当年7月降水含有2.34~2.68年,4.92年,5.26年的显著周期,可能与ENSO活动有关。     

北疆黄土的磁化率各向异性揭示末次冰期以来古风向的变化

黄土磁化率各向异性（AMS）被认为是重建古风向变化重要的指标之一,在黄土高原地区得到广泛的应用。然而新疆地区的黄土磁化率各向异性研究相对薄弱。通过对新疆塔城盆地库尔托别剖面磁化率各向异性参数和磁化率分析古风向和风力强度的变化,结果表明：塔城地区末次冰期以来以东南风为主,剖面从下至上,可分为5个阶段：第1阶段（12~14 m）：对应MIS3c时期,磁组构特征受水流作用的影响明显,表现为东南风。第2阶段（6~12 m）：对应MIS3b时期,出现西南风,但主要还是以东南风为主。第3阶段（4~6 m）：对应MIS3a早中期,以东南风为主,西南风逐渐消失,并且风力强度逐渐减弱。第4阶段（0.5~4 m）：对应MIS3a晚期和MIS2早期,表现为东南风,风力强度波动较大。第5阶段（0~0.5 m）：磁组构特征受成壤作用影响强烈。     

檀头山海底电缆路由工程地质条件及评价

在浙江象山檀头山海底电缆路由勘察中获得的地形测量、侧扫声纳和浅地层剖面探测、工程地质钻探等资料基础上,结合其他自然环境资料对路由勘察区工程地质条件进行了详尽的分析和研究。结果表明,该区域工程环境较适合海缆的铺设,海缆可铺设于勘察区的南部,登陆点附近基岩裸露区和砾石应进行清理、开挖和采取防护措施,海底和冲刷槽边坡稳定,檀头山附近水下浅滩地层中浅层气上冲至海底面以下最浅不足5m,对海底电缆影响不大,但要在开挖施工时引起注意。     

Stratospheric Aerosol Extinction Profile Retrieval from SCIAMACHY Limb Measurements

Stratospheric aerosol extinction profiles are retrieved from Scanning Imaging Absorption Spectrome- ter for Atmospheric Cartography （SCIAMACHY） limb scatter measurements. In the process of retrieval, the SCIATRAN radiative transfer model is used to simulate the limb scattering radiation received by the SCIAMACHY instrument, and an optimal estimation algorithm is used to calculate the aerosol extinction profiles. Sensitivity analy- ses are performed to investigate the impact of the surface albedo on the accuracy of the retrieved aerosol extinction profiles in the northern midlatitudes. It is found that the errors resulting from the bias of the assumed surface albedo in the retrieval are generally below 6%. The retrieved SCIAMACHY aerosol extinction profiles are compared with corresponding Stratospheric Aerosol and Gas Experi- ment （SAGE） II measurements, and the results indicate that for the zonal mean profiles, the SCIAMACHY retrievals show good agreement with SAGE II measurements, with the absolute differences being less than 2.3 × 10-5 km-1 from 14-25 km, and less than 5.9×10-6 km-1 from 25-35 km; and the relative differences being within 20% over the lati- tude range of 14-35 km.     

Models for Estimation of Single Leaf Area of Mangrove TreesModels Trees based on Leaf Length and Widthbased Width

Leaf area is an important parameter for modeling plant growth and physiological processes.It is very expensive and difficult for measuring leaf area by means of Leaf Area Meter,therefore,it’s quite necessary to obtain one simple model for estimation of leaf area of mangrove tree.The models for estimation of leaf area of 3 species of mangrove trees were developed based on leaf length and width.Totally,leaf area(LA),leaf length(L)and width(W)were measured from 450 fresh leaves of major three species of mangrove trees in Zhangjiang Estuary Mangrove National Natural Reserve,Fujian province.The actual leaf area of the plant was measured with the help of ArcGIS software and regression model was fitted.The majority of the data(80%)were used for model calibration,and the remaining data(20%)were used for model validation.All the leaf areas of 3 species of mangrove trees had been significant correlation between L,W,L·W,L2,W2and(L+W)2,so the factors could be constructed into a regression model with leaf area.Six models for estimation of leaf area selected were significantly(p0.001)regressed with L,W and the functions of these dimensions.All models were linear relationships.Based on goodness of fit,prediction ability and residual performance,it was found that model 3 could best describe the relationship between leaf area and leaf length and width.By means of regression analysis,the following models were developed:LA=0.28+0.66L·W(R2=0.980)for Kandelia candel,LA=0.09+0.73L·W(R2=0.983)for Avicennia marina,LA=0.52+0.72L·W(R2=0.990)for Aegiceras corniculatum,respectively.The study provided a simple,reliable and non-destructive method for estimating single leaf area.It had a good potential in the functional structural model of mangrove tree.     

一种阵列式海洋磁力测量系统

基于多台海洋磁力仪、测深仪和GPS,研制了数据合成器、水下拖体、电源适配器、数据收录兼导航软件,最终构建了一种阵列式海洋磁力测量系统。该阵列式海洋磁力测量系统具备3个磁力仪通道,动态噪声≤0.3n T p-p,采样率为10Hz,水下部分总重量≤95kg,配迫降翼后入水深度可达22m。该阵列式磁力测量系统曾被应用于董家口港区某锚地的未爆炸物探测,最终确定了多个疑似物位置。