Dissolved organic matter in surface runoff in the Loess Plateau of China: The role of rainfall events and land-use

Exploring the chemical characterization of dissolved organic matter (DOM) is important for understanding the fate of laterally transported organic matter in watersheds. We hypothesized that differences in water-extractable organic matter (WEOM) in soils of varying land uses and rainfall events may significantly affect the quality and the quantity of stream DOM. To test our hypotheses, characteristics of rainfall-runoff DOM and WEOM of source materials (topsoil from different land uses and gullies, as well as typical vegetation) were investigated at two adjacent catchments in the Loess Plateau of China, using ultraviolet–visible absorbance and excitation emission matrix fluorescence with parallel factor analysis (PARAFAC). Results indicated that land-use types may significantly affect the chemical composition of soil WEOM, including its aromaticity, molecular weight, and degree of humification. The PARAFAC analysis demonstrated that the soils and stream water were dominated by terrestrial/allochthonous humic-like substances and microbial transformable humic-like fluorophores. Shifts in the fluorescence properties of stream DOM suggested a pronounced change in the relative proportion of allochthonous versus autochthonous material under different rainfall patterns and land uses. For example, high proportions of forestland could provide more allochthonous DOM input. This study highlights the relevance of soils and hydrological dynamics on the composition and fluxes of DOM issuing from watersheds. The composition of DOM in soils was influenced by land-use type. Precipitation patterns influenced the proportion of terrestrial versus microbial origins of DOM in surface runoff. Contributions of allochthonous, terrestrially derived DOM inputs were highest from forested landscapes.     

Development of Land Resources in Transitional Zones Based on Ecological Security Pattern: A Case Study in China

Land use based on landscape ecological security pattern provides a scientific basis for alleviating conflicts between land conservation and human use, ensuring concomitant economic development and ecological integrity. The majority of studies by Chinese researchers have been focused on the carrying capacity and land development intensity, and less attention has been paid to the ecological security pattern of the landscape in Mianzhu in the transitional zone between the Chengdu Plain region and the Longmen Mountains, western China. However, land resources are undergoing significant changes resulting from land use associated with rapid economic development and demographic growth. In this study, we constructed a minimum cumulative resistance model in Mianzhu in the transitional zone, and the land space was divided into optimized development areas, key development areas, restricted development areas, and prohibited development areas according to the landscape ecological security pattern based on the model surface. These land use types covered 7218.39 ha, 17,974.75 ha, 21,545.39 ha, and 77,791.46 ha, respectively. We also examined land use changes over the last 20 years and quantitatively analyzed the relationships between land use changes and geographic factors based on remote sensing and geographic information system. The information obtained from this research ultimately impacts future policies and plans regarding land resources and can be used to promote the sustainable use of land resources in the region.

     

Multiple overpressure systems and their relationship with hydrocarbon accumulation in the Qikou Depression of the Bohai Bay Basin,China

Pressure measurements using drill stem tests and estimates from log data calculation indicate that three vertically stacked regional pressure compartments exist in the Qikou Depression of Bohai Bay Basin, N. China. The compartments comprise hydrostatic, upper weak, and lower overpressure systems. Laterally, overpressure (pressure coefficient > 1.2) occurs in the deeper areas and weakens gradually from the centre to the margin of the depression. The accumulation of oil and gas exhibits the interesting characteristics of oil‐bearing layers above gas‐bearing layers in the Qikou Depression. The pattern can be accounted for by the evolution of overpressure system, the maturity process of the source rock and the main fault activity. In the late Dongying Formation (Ed, 30 Ma), the lower overpressure system began to form shape, and the hydrocarbon sources generated a large volume of oil. However, because there was no migration pathway, the oil only accumulated in the original strata. In the late Guantao Formation (Ng, 12 Ma), the gas was generated, the upper overpressure system formed gradually, and the activity of the main fault gradually increased. Then, the overpressure pushed the early gathered oil to flow from the lower overpressure system into the upper overpressure system. Afterwards, the activity of the main fault decreased again and remains weak until now. Thus, later generated natural gas cannot keep migrating along the main fault and can only accumulate in the lower overpressure system. Copyright © 2014 John Wiley & Sons, Ltd.     

重要性权值的驾车导航POI表达规则

在导航电子地图中,针对驾车任务的POI自适应表达是提高导航电子地图信息传输效率的关键。针对这一问题,提出了基于重要性权值的驾车导航POI表达规则。首先,分析了POI重要性权值的影响因素;其次,从影响因素出发,研究了基于权值的POI规则表达的各规则项;最后,设计了POI自适应表达规则库,并在嵌入了数据处理规则库的绘图软件上进行了技术实现。试验结果表明,利用基于权值的POI表达规则进行地图表达,可以提高地图内容的层次性与清晰性,优化驾车导航服务。     

大别山晓天—磨子潭韧性剪切带主要造岩矿物的变形与应变分析

大别山北缘的晓天—磨子潭韧性剪切带主体发育在北大别片麻岩之上,具有近水平左行剪切的运动学特征;剪切带自中心向外围依次发育超糜棱岩、糜棱岩、初糜棱岩、变形片麻岩(片岩)、围岩,发生变形的主要造岩矿物包括石英、长石、角闪石、云母等。岩石有限应变测量和矿物颗粒形态学优选方位统计显示,随着糜棱岩化程度的加强,主要造岩矿物平均粒径均呈递减变化;矿物长短轴所反映的应变均呈加强的趋势,矿物长轴与X的锐夹角皆逐渐变小;以90°为一个区间统计的矿物长轴定向显示,变形矿物的长轴在钝角区间(顺剪切方向)有优选,以15°为一个区间统计的矿物长轴定向显示,矿物定向存在一定对称性,即在锐夹角区的优选区间和钝夹角区的优选区间互为补角区间。此外,云母矿物的应变在不同样品中均显示最大,其次为石英、角闪石、长石;随着构造岩类型的不同,应变的变化趋势最明显的也是云母,其次为石英,角闪石和长石变化不明显;矿物长轴与X轴夹角的统计表明,云母、角闪石长轴与X轴锐夹角比石英、长石均偏小。矿物的变形还表明,指示剪切带剪切方式最明显的是云母类矿物,尤其是云母鱼构造,是判定运动方向的可靠标志,其次是角闪石,较之斜长石更易形成不对称残斑构造;综合矿物在剪切带中的含量和分布,结构特点,以及对剪切带应变反映的"灵敏性"等方面的因素,石英矿物最能表现剪切带的整体应变状态,是较为理想的应变标志矿物。上述结果表明不同矿物随变形环境的渐变,在粒径、应变、形态学优选等方面具有较统一的变化,即不同变形矿物在反映剪切带的剪切作用方式、应力—应变等特征时是较为一致的;同时不同矿物在上述变化中又表现出区别于其他矿物的各自特点,这反映了矿物自身的晶体结构、结晶形态、力学性质、变形习性等特性。所以,对于研究韧性剪切带而言,针对不同研究内容,要综合不同矿物的变形情况来选取合适的变形矿物及其变形组构来研究,才能得到更准确的结果和更合理的解释。     

博格达山东段苏吉山辉长岩LA-ICP-MS锆石U-Pb年龄、地质地球化学特征及构造意义

苏吉山辉长岩体位于博格达碰撞造山带东段,卡拉麦里蛇绿混杂岩带西南侧,出露面积约1.8 km~2,岩性为石英角闪辉长岩。苏吉山辉长岩体富含普通角闪石(20%)和磁铁矿物,表明原生岩浆富水、高氧逸度特征,岩石化学组成属于拉斑玄武岩系列,岩石弱富集大离子亲石元素Cs、Rb、Ba、Th、U,显著亏损Nb、Ta、Zr、Hf和弱亏损Ti,显示源区为受俯冲流体交代改造的岩石圈地幔,应是洋壳俯冲的产物。苏吉山辉长岩体锆石U-Pb年龄为308.1±3.3Ma,早于卡拉麦里混杂岩带内碱性花岗岩侵位,介于博格达裂谷活动期,是裂谷作用由全面伸展向局限伸展转换的标志。苏吉山辉长岩空间上位于古亚洲洋板块沿卡拉麦里蛇绿混杂岩带向准噶尔板块斜向俯冲的前进方向,时间上介于博格达裂谷活动期,地球化学上显示洋壳俯冲的特征,各种事实表明,古亚洲洋沿卡拉麦里碰撞带向准噶尔板块斜向俯冲作用形成撕裂型博格达裂谷,博格达裂谷由伸展机制向伸展-碰撞过渡机制的应力调整导致了苏吉山辉长岩体的侵位。     

华北克拉通乌拉山地区早前寒武纪岩浆作用和变质作用——锆石SHRIMP U-Pb定年及岩石地球化学研究

乌拉山地区位于大青山地区西侧,变泥砂质岩石大范围出露,并有一定数量变质岩浆侵入岩存在。本文对6个变质岩浆侵入岩进行了锆石SHRIMP U-Pb定年。片麻状闪长岩、片麻状英云闪长岩、片麻状花岗闪长岩和片麻状紫苏花岗岩等4个样品的锆石U-Pb数据点沿谐和线分散分布,n(~(207)Pb)/n(~(206)Pb)年龄从约2.5Ga到约1.8 Ga。变质辉长岩和眼球状石英二长岩锆石U-Pb数据点在谐和线上较集中分布,n(~(207)Pb)/n(~(206)Pb)年龄从约2.0Ga到约1.8 Ga。n(~(207)Pb)/n(~(206)Pb)年龄越小的锆石域通常显示越强烈的重结晶。结合已有研究和地球化学资料,可得出如下结论。(1)乌拉山地区存在新太古代晚期(约2.5 Ga)和古元古代中晚期(约2.0 Ga)岩浆侵入岩,后者形成于伸展构造环境。(2)乌拉山地区遭受新太古代晚期一古元古代早期和古元古代晚期两期构造热事件叠加改造。(3)乌拉山地区部分变泥砂质岩石形成于新太古代晚期,大青山地区原认为形成于古元古代早期的"大青山表壳岩"很可能也形成于新太古代晚期。(4)乌拉山地区和大青山具有类似或相同的早前寒武纪地质演化历史。