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排序方式: 共有358条查询结果,搜索用时 15 毫秒
81.
Haris Ahmed KHAN Ali Asghar SHAHID Muhammad Jahangir KHAN Taher ZOUAGHI Maria Dolores ALVAREZ Syed Danial Mehdi NAQVI 《《地质学报》英文版》2023,97(1):256-268
This research is focused on the analysis of the sequence stratigraphic units of F3 Block, within a wave-dominated delta of Plio–Pleistocene age. Three wells of F3 block and a 3D seismic data, are utilized in this research. The conventional techniques of 3D seismic interpretation were utilized to mark the 11 surfaces on the seismic section. Integration of seismic sequence stratigraphic interpretation, using well logs, and subsequent 3D geostatistical modeling, using seismic data, aided to evaluat... 相似文献
82.
Tao He Mufei Li Zhaochu Hu Wen Zhang Haihong Chen Zaicong Wang Yongsheng Liu 《Geostandards and Geoanalytical Research》2023,47(1):155-168
The lack of analytical techniques for halogens in geological materials is mainly due to the loss of analytes during sample preparation. This study describes a rapid bulk rock digestion method (NH4F digestion) for determination of the abundances of Cl, Br and I in geological materials by SF-ICP-MS. During high temperature (200–240 °C) digestion, NH3 released from the decomposition of molten NH4F can effectively prevent the loss of halogens released from geological samples. Chlorine, Br and I were not lost during NH4F digestion at 220 °C for 0.25–6 h. The limits of quantitation for NH4F digestion were 2.8, 0.018 and 0.003 μg g-1 Cl, Br and I, respectively. Most results for halogens in geological reference materials by NH4F digestion were in agreement with their certified values, confirming that the high-performance rapid bulk rock NH4F digestion has sufficient digestion capability to extract Cl, Br and I from rocks, sediments and soils. In comparison, results obtained following acid digestion showed that HNO3 + HF digestion could effectively extract Br and I from soil and sediment samples, and that HNO3 acid digestion is only suitable to use for the determination of Br and I in soil samples. 相似文献
83.
Phylogeography of Ophryotrocha labronica (Polychaeta,Dorvilleidae) along the Italian coasts
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Piero Cossu Ferruccio Maltagliati Federica G. Pannacciulli Roberto Simonini Gloria Massamba‐N'Siala Marco Casu Claudio Lardicci Daniela Prevedelli Alberto Castelli 《Marine Ecology》2015,36(4):1088-1097
Species of the genus Ophryotrocha are a well‐studied group of organisms but, despite the relatively large body of biological studies, little is known about their intra‐specific patterns of genetic diversity. In the present study, we analysed the patterns of genetic variation in samples of Ophryotrocha labronica (Polychaeta, Dorvilleidae) collected along the Italian coasts within three regions with different thermal regimes: the Northern Adriatic Sea (NAS), the Ligurian Sea (LS), and the South/Southeast Sicilian Sea (SS). A partial sequence of the cytochrome c oxidase subunit I (COI) gene was used as a genetic marker. An analysis of molecular variance (AMOVA) showed significant genetic differentiation between the NAS and the other regions. Conversely, little or no genetic structuring was found between the LS and the SS or amongst locations within a given region. A Bayesian phylogenetic tree and a median‐joining network provided evidence for the occurrence of two highly divergent genetic lineages characterized by a high average sequence divergence (17.2%, Kimura two‐parameter distance). The spatial patterns of genetic variation found in O. labronica may reflect the signature of past expansion events of the two genetic lineages. Although the high sequence divergence suggested that cryptic speciation within O. labronica may have occurred, other traits such as the absence of reproductive isolation, pattern of phenotypic variation and habitat specificity prompted us to regard the two groups as distinct COI lineages of O. labronica. 相似文献
84.
笔者结合珠江三角洲地区和中国土壤含F背景,研究了该区土壤F的含量特征、总体和典型区域的分布状况,对土壤类型、成土母质和土地利用类型等影响因素进行了分析,初步探讨了土壤F与地氟病的关系。结果表明,珠江三角洲地区浅层、深层土壤F平均含量分别为510mg/kg和529mg/kg,其中海(陆)相第四纪松散层区的三角洲沉积潜育性水稻土、三角洲盐渍水稻土、基水地的F含量最高。6760km2的浅层土壤F高背景区广泛分布于平原区,东莞、新会、珠海局部呈现污染区;深层土壤F高背景区5504km2,而污染区都集中在邻海的珠海市高栏、三灶两岛。土壤F的富集在沉积物区明显与第四纪海陆、陆海交互相沉积物有关,在基岩区明显和花岗岩类有关,人类影响较强的土壤和水稻土及其盐渍化有利于F富集。区内地氟病分布于从化、增城、东莞郊区、南海、新会和恩平,病区均位于高F的地层岩石区和土壤高F区。土壤F高背景区生长的农作物F含量存在超标,且病区农作物F超标率和超标倍数大于非病区,表明土壤中F的生物有效量比例较高,土壤F已向农产品中迁移和富集,危及到农产品质量。高F的地质环境是造成本区土壤及其农作物F含量高的主要原因,成为地氟病发生的致病因素。 相似文献
85.
磷灰石结构通道离子对晶胞参数的影响 总被引:8,自引:1,他引:8
磷灰石晶胞参数受其结构中Ca多面体,磷氧四面体及结构通道位置上的类质同角替换的影响,本文探讨了54个磷灰石样吕的晶胞参数与结构通道离子F,OH,Cl相同象替换的影响,本文讨论了54个磷灰石样品的晶胞参数与结构通道离子F,OH,Cl相对含量的关系,发现Cl和取代是影响岩浆型磷灰石晶胞参数的主要因素,每原子/晶胞的Cl使a增大0.121 1(6)nm,c减少0.0633 (3)nm,根据成分与结构的经验关系式,可以验证电子探针对F的分析结果。 相似文献
86.
Polychlorinated Dibenzo-p-dioxins, -furans (PCDD/F) and Analogues in Surface Sediments and Dated Aquatic Sediment Cores Aquatic sediments are the final sinks of unintentionally formed PCDD/Fs. Still not known are the conditions of formation of PCDD/Fs in the 8120 years old sediments in Japan and in 350 to 400 years old sediments in the Baltic. Sediments are means of source identification if transformation processes are taken into consideration in view of hydrological conditions. PCDD/Fs have been analysed 30 km from the source in sediments and over a distance of 50 km in benthos indicating a remarkable bioaccumulation potential. Elaborated data of the PCDD/F sediment contamination are missing as well as information on internal diagenetic processes, interactions at the sediment/water interface, and on the aerobic and anaerobic biodegradation and bioavailability of PCDD/Fs in sediments. Quality criteria for sediments and aquatic ecosystems remain to be elaborated. 相似文献
87.
黄河矿 BaCe(CO3)2F(a=0.5072(1)nm,c=3.846(1)nm;V=856.8×10-3nm3;Z=6)晶体结构的重新测定,采用中心对称空间群 R3m-D3d5,基于337个可观察的单晶 X 射线数据(I>2σ1)和30个可变参数,R=0.031。原子坐标和均方根振幅(据各向异性位移参数计算,O.013-0.025nm)表明,没有必要降低对称性,即没有必要采用相应的非中心对称空间群或其它次群。黄河矿的结构中,原子形成似层状排列,且垂直于 c 轴;碳酸根通过 Ba 与 Ce 的联结形成三维结构。C(1)O3,和 C(2)O3,中的 C 原子偏离三个氧组成的平面,其偏离的距离分别为0.0066(15)nm 和 0.0029(15)nm。 相似文献
88.
CLM在淮河流域数值模拟试验 总被引:8,自引:1,他引:8
文中利用 1998年HUCEX资料对CommonLandModel(CLM )的模拟能力进行了验证。结果表明 ,CLM不但能够较好地模拟陆 气间各种能量通量 ,而且还能模拟出土壤中温度的时空分布特征。春季 ,CLM对潜热模拟偏高 ,从而引起土壤温度模拟偏低 ;而在夏季 ,潜热模拟偏低 ,在旱地下垫面由于净辐射模拟偏低使土壤温度的模拟仍然偏低 ,水田下垫面的土壤温度模拟趋向合理。夏季的水田无论在对大气的能量输送还是土壤的温度分布上 ,都有其特殊性 ,需在陆面模式中予以特殊的考虑。 相似文献
89.
水文变异的滑动F识别与检验方法 总被引:20,自引:1,他引:20
针对传统F检验法只能用于已知变异点的检验,而无法用于变异点的识别问题,本文提出了滑动F识别与检验法。该法首先利用传统F检验法对序列逐点进行检验,找出满足F计算值大于临界值的所有可能变异点,然后选择F计算值达到最大值的那一点作为最可能变异点。利用该法对潮白河水资源分区45年年径流量序列进行了分析,并从物理成因角度对该检验结果进行了确认。结果表明滑动F 识别与检验法具有较好的检验效果,检验结果可信度较高。 相似文献
90.