From 2D to 3D Modeling of Mineral Prospectivity Using Multi-source Geoscience Datasets,Wulong Gold District,China

Natural Resources Research - The Wulong gold district (WGD) is located at the northeastern margin of the North China Carton (NCC) on the Liaodong Peninsula, China. The results of early mineral...     

Bulk organic δC and C/N as indicators for sediment sources in the Pearl River delta and estuary,southern China

Preservation of organic matter in estuarine and coastal areas is an important process in the global carbon cycle. This paper presents bulk δ¹³C and C/N of organic matter from source to sink in the Pearl River catchment, delta and estuary, and discusses the applicability of δ¹³C and C/N as indicators for sources of organic matter in deltaic and estuarine sediments. In addition to the 91 surface sediment samples, other materials collected in this study cover the main sources of organic material to estuarine sediment. These are: terrestrial organic matter (TOM), including plants and soil samples from the catchment; estuarine and marine suspended particulate organic carbon (POC) from both summer and winter. Results show that the average δ¹³C of estuarine surface sediment increases from −25.0 ± 1.3‰ in the freshwater environment to −21.0 ± 0.2‰ in the marine environment, with C/N decreasing from 15.2 ± 3.3 to 6.8 ± 0.2. In the source areas, C₃ plants have lower δ¹³C than C₄ plants (−29.0 ± 1.8‰ and −13.1 ± 0.5‰ respectively). δ¹³C increases from −28.3 ± 0.8‰ in the forest soil to around −24.1‰ in both riverbank soil and mangrove soil due to increasing proportion of C₄ grasses. The δ¹³C_POC increases from −27.6 ± 0.8‰ in the freshwater areas to −22.4 ± 0.5‰ in the marine-brackish-water areas in winter, and ranges between −24.0‰ in freshwater areas and −25.4‰ in brackish-water areas in summer. Comparison of the δ¹³C and C/N between the sources and sink indicates a weakening TOM and freshwater POC input in the surface sedimentary organic matter seawards, and a strengthening contribution from the marine organic matter. Thus we suggest that bulk organic δ¹³C and C/N analysis can be used to indicate sources of sedimentary organic matter in estuarine environments. Organic carbon in surface sediments derived from anthropogenic sources such as human waste and organic pollutants from industrial and agricultural activities accounts for less than 10% of the total organic carbon (TOC). Although results also indicate elevated δ¹³C of sedimentary organic matter due to some agricultural products such as sugarcane, C₃ plants are still the dominant vegetation type in this area, and the bulk organic δ¹³C and C/N is still an effective indicator for sources of organic matter in estuarine sediments.     

抚州市生态系统气象利用价值核算方法

采用抚州市2017—2021年各县（区）气温、降水、日照、风速等气象资料和年鉴统计资料,从气象角度对生态系统的 产品供给利用服务、调节服务和文化服务功能三方面建立生态系统气象利用价值核算方法。结果表明：1）抚州全市生态系 统气象利用价值为233亿元,约为全市年平均GDP 的15.3%。核算指标中,气象供给利用服务价值最高,为219.16亿元,占 总价值的 94.1%;其次为气象文化服务价值,为 12.83 亿元,占总价值的 5.5%。2）抚州市生态系统气象利用价值以临川区 61.16亿元最高,占全市的26.3%;广昌县8.82亿元最少,占全市的3.8%。研究结果可为地方政府和有关部门加强生态保护 规划和推进生态产品价值实现工作提供参考和依据。     

基于引潮力附加构造应力调制的九江 地震热异常时空动态过程研究

通过利用发震区域的天体引潮力附加构造应力变化模型, 研究了2005年11月26日江西九江M_S5.7地震发震构造与天体潮汐引力的关系, 并利用该模型结合美国国家环境预报中心多源综合温度数据资料, 分析了九江地震前后发震区域热异常在时空上的动态变化特征. 结果显示, 一方面, 在时间序列变化上, 孕震区热异常表现出的起始—消亡演变过程与岩石在应力加载下的形变—破裂过程相吻合. 无论近地表大气还是上附多层大气, 热异常主要集中在活动断裂带及其附近区域, 与构造断裂带分布相一致; 同时, 热异常从近地表到高空消失的垂向分布, 符合地面对大气加热导致大气升温→抬升→扩散→消亡的大气动力学基本特性, 表明构造运动是本次温度异常变化的主控原因. 另一方面, 热异常变化遵循引潮力(低值—高值—低值)的变化过程, 显示出天体引力对发震断层温度异常识别具有一定的指示意义以及引潮力可能对构造应力处于临界状态的发震断层具有诱震作用, 预示利用引潮力附加构造应力与热异常变化相结合研究短临地震预测具有一定价值.     

1999-2018年重庆市主城区住宅用地空间演变特征及驱动因素研究

以典型山地城市重庆市主城区为研究对象,基于住宅小区空间矢量数据和多源兴趣点(Point of Interest,POD数据,采用标准差椭圆、圈层缓冲区分析、扩展强度指数、景观格局分析和地理加权回归(GWR,Geographic-ally Weighted Regression)方法,对近20 a重庆市主城区住宅小区的空...     

水文地质数值计算的自动实现

水文地质数值计算的自动实现纵建平（煤炭科学研究总院西安分院水文所７１００５４）关键词水文地质,数值计算,重定向技术,自动化中国图书资料分类法分类号ＴＰ３１１作者简介纵建平男３８岁工程师水文地质数值法目前已成为水文地质工作者进行地下水流场分析、煤矿涌水...     

灵渠地质地貌初步研究

灵渠位于广西东北部的兴安县,建造于公元前214年的秦朝,是联接湘江和漓江的一条人工运河。灵渠的建造是利用了分水岭上特定的有利的地质—地貌条件,即:1.地质构造上的低点;2.分水岭上强烈喀斯特化的峰林平原地形;3.从漓江到湘江新构造运动为掀斜式上升。     

武汉志留纪兰多维列世盔甲鱼类新材料

汉阳鱼作为湖北武汉地区古生代鱼类的代表,其真实形态一直未被确定下来,同时关于汉阳鱼目内部的系统发育学关系也只停留在其下两个属种的讨论上,并未对其开展详细的分析讨论.采用形态学和分支系统学的方法,对湖北武汉兰多维列世清水组上部的盔甲鱼类新材料进行了详细研究,建立了汉阳鱼科一新属新种:意外洪山鱼(Hongshanaspis...     

Late Devensian and Holocene relative sealevel changes at Loch nan Eala,near Arisaig,northwest Scotland

Pollen, diatom, radiocarbon and lithostratigraphical data from isolation basins in northwest Scotland are used to quantify the reference water (tide) level, indicative range and age of differenty types of isolation and connection contacts. Tendencies of sea-level movement and relative sea-level changes from the mid-Lateglacial Interstadial (11.8 ka BP) to the late Holocene are constructed from these data. Relative sea-level fell continuously from + 17.8 m OD at 11.8 ka BP to ca. + 5.2 m OD at 10.1 ka BP. From an unkown minimum between 10 ka and 9 ka BP relative sea-level then rose to +6.3 m OD at 8.3 ka BP. The maximum Holocene sea-level occurred within the range +6.6 m OD to +9.3 m OD between 6.6 ka BP and 4.0 ka BP before falling to present. Isobase, age-altitude and quantitative rebound models for northwest Scotland are tested using these sealevel data, but none of the published models shows close agreement with the new results.     

黄土深基坑边坡稳定的实例分析

应用泰勒（Ｔｏｙｌｏｒ）理论，对黄土地基边坡稳定实例分析，并对边坡土样做快速直剪试验，一定程度揭示了均质粘性上边坡稳定的内涵。