浙江诸暨地区石角-璜山侵入岩LA-ICP-MS锆石U-Pb年龄——对超镁铁质球状岩成因的启示

对分布于江南造山带东段江绍断裂带附近的浙江诸暨地区石角-璜山侵入岩进行了LA-ICP-MS锆石U-Pb定年工作,石角角闪辉石岩和璜山石英闪长岩的结晶年龄分别为844Ma±3Ma和818Ma±6Ma。该年龄结果表明,石角村附近的超镁铁质岩(包括球状辉闪岩)与其外围的闪长岩可能并非同时形成。江绍断裂带附近分布的多个闪长岩体的形成时代介于930~820Ma之间。对这些超镁铁质岩和闪长岩的精细岩石成因研究将有助于揭示扬子和华夏在新元古代时期的拼接过程。     

二维随机介质模型正演指导复杂地层地震解释——以薄层砂泥岩交互地层为例

大港油田砂泥岩交互地层存在着非均质复杂地质形态,为保证其精细解释效果,根据随机过程理论,提出了选用二维指数型椭圆自相关函数为复杂非均质地质体进行简化建模的方法。正演算法使用交错网格有限差分法模拟弹性波在二维随机介质模型中的传播,激发方式使用自激自收模式。正演结果表明,随机介质模型模拟大港油田薄层砂岩互层地层具有合理性,交错网格有限差分算法对于该模型的正演数值模拟,算法合适。     

活动断裂引发的环境地质问题及措施

随着经济的飞速发展和现代化建设的加快，全社会防灾减灾意识的增强，在国土规划、抗震规划及高、深、大型工程项目的建设中，对活动断裂的研究，已成为勘测、设计中的重要课题。本文就影响张家口市城市安全的活动断裂的类型、空间展布、活动特征、引发的环境地质灾害及工程对策等予以阐述，为城市规划提供依据。     

成都粘土路堑边坡防护研究

成都外环路高速公路东半环超过有20km的路段处在成都粘土分布区，针对成都粘土的易滑性，本文提出了全封闭的浆砌片石护坡，土钉墙，非全封闭的锚杆框架护坡，钢纤维混凝土喷锚全封闭护坡，重力式挡土墙等五种方法处理成都粘土路堑边坡工程，施工实践表明，这些方法行之有效，在该类土的边坡防护中值得推广。     

基于RS和GIS的新疆渭干河三角洲的耕地及盐渍化分析

渍化耕地面积为16.68×104 hm2,占耕地总面积的54.47%.耕地盐渍化现象普遍,主要分布在绿洲的下部边缘地带,河流中下游、地势平缓低洼等区域.盐渍化耕地呈条形状分布,在绿洲边缘带呈片状分布,边缘的重度盐渍化耕地交错分布在轻度和中度盐渍化耕地中;3)自然因素是导致耕地盐溃化的前提和物质基础,人为因素是盐渍化形成及发展的重要驱动力.     

Relation between temperature changes of the mid-upper troposphere over Eurasian mid-high latitudes and solar irradiance in the twentieth century

The δ¹⁸O data obtained from an 18.7 m ice core drilled in Chongce Ice Cap at an elevation of 6,530 m a.s.l. in the West Kunlun Mountains on the northern Tibetan Plateau show a strong correlation with the summer temperature of the middle to upper troposphere over the mid-high latitudes of Eurasia. Based on this, the δ¹⁸O record can be used as a proxy of the June–September mean temperature of the mid-upper troposphere (MUT) from 1903 to 1992. The time span of the ice core record is much longer than the meteorological data available only after 1948. Using the empirical mode decomposition method (EMD), the δ¹⁸O record is decomposed into various frequency components and compared with the solar irradiance variations of the same period. The results show that (1) The June–September mean temperature of the MUT over Eurasian mid-high latitudes is completely decomposed into four IMF (intrinsic mode function) components and an increasing trend. (2) Solar irradiance is decomposed into the Schwabe cycle, the Hale cycle, the Gleissberg cycle, and an increasing trend. (3) The correlation coefficients between the June and September mean temperatures of the MUT over Eurasian mid-high latitudes and solar irradiance on the longer timescales (at least more than 11-year) show the significant correlations; their phase changes are basically identical in general, and (4) the 11-year Schwabe cycle exists in the June–September mean temperature of the MUT over Eurasian mid-high latitudes during most of the time from 1903 to 1992, and only in the two high-temperature phases (1929–1944 and from 1975 to the present) may global warming disturb this relation. A full understanding of this phenomenon would shed insight into the potential consequence of global warming on the MUT.     

钱塘江江心排污的数值模拟

从立面二维非恒定流体动力学方程出发,应用κ-ε湍流模式计算流场,再用准三维的浓度对流-扩散方程,即考虑了侧向扩散的立面二维浓度控制方程,模拟了钱塘江江心6个竖管排污在潮流作用下近区浓度场,其结果和实际观测值基本吻合。     

地质雷达在隧道检测中的应用

隧道施工完成后用常规方法很难对衬砌质量做出系统评价，地质雷达利用超高频脉冲电磁波探测目标介质的介电常数，很容易掌握砼衬砌结构的厚度、衬砌周围回填及空隙情况，围岩断层裂隙构造情况等，为工程技术评价提供依据。文章以实例，介绍了利用地质雷达对隧道进行检测所使用的仪器、工作参数及地质雷达资料处理解释步骤，并通过对几幅典型雷达图像进行分析介绍了不同异常结构在雷达剖面上的反映。     

Estimation of the minimum food requirement using the respiration rate of medusa of Aurelia aurita in Sihwa Lake

We examined the respiration rate of Aurelia aurita medusae at 20 °C and 28 °C to evaluate minimum metabolic demands of medusae population in Sihwa Lake, Korea during summer. While weight specific respiration rates of medusae were constant and irrespective to the wet weight (8?C220 g), they significantly varied in respect to temperatures (p<0.001, 0.11±0.03 mg C g^?1 of medusa d^?1 at 20°C and 0.28±0.11 mg C g^?1 of medusa d^?1 at 28 °C in average, where Q ₁₀ value was 2.62). The respiration rate of medusae was defined as a function of temperature (T, °C) and body weight (W, g) according to the equation, R=0.13×2.62^(T-20)/10 W ^0.93. Population minimum food requirement (PMFR) was estimated from the respiration rate as 15.06 and 4.86 mg C m^?3 d^?1 in June and July, respectively. During this period, increase in bell diameter and wet weight was not significant (p=1 in the both), suggesting that the estimated PMFR closely represented the actual food consumption in the field. From July to August, medusae grew significantly at 0.052 d-1, thus the amount of food ingested by medusae population in situ was likely to exceed the PMFR (1.27 mg C m^?3 d^?1) during the period. In conclusion, the medusae population of higher density during June and July had limited amount of food, while those of lower in July and August ingested enough food for growth.