一种用于海洋综合观测浮标的多种通信方式集成系统

为了优化海洋综合观测浮标的通信系统,设计了一种通信方式集成系统,将多种通信模块进行集成管理,并在每个数据发送周期进行通信信号检测,经过比较选择最优的通信方式进行数据传输。该系统具有采集数据完整、数据冗余小、运行功耗低等优点,有效增强了浮标的通信能力,完善了原有通信系统的功能,并且后期还具备较强的可扩展性功能,如浮标舱内环境监测和独立定位等,进一步增强浮标的安全性。该系统已经完成12个月的海上试运行,系统运行稳定,功能达到预期,可满足海洋综合观测浮标对多种通信方式进行优化管理的需求。     

茂名建设现代化海洋经济体系的现状、问题及路径

在广东实现“四个走在全国前列”的时代需求下,茂名应着力建设现代化海洋经济体系。近年来,茂名海洋经济总量快速增长、海洋经济体系基本形成、海洋创新成果初具规模、海洋生态建设成效显著、海洋管理能力不断增强,奠定了建设现代化海洋经济体系的基础,但也面临着海洋经济规模偏小且结构不够合理、现代化海洋产业进程缓慢、现代化海洋经济发展动力不足且受到制约和缺乏保障等问题。未来应从加快供给侧改革、实施创新驱动、推进开放合作、优化海洋生态系统和完善体制机制等方面寻求茂名建设现代化海洋经济体系的路径策略。     

基于博弈论的海洋渔业融资约束问题研究

疫情的冲击使社会经济发展受到影响,我国政府出台一系列激励性政策,力求恢复企业正常生产经营。然而要实现金融支持的精准投放,亟须厘清目前海洋渔业融资约束形成的原因,从而有的放矢。文章在博弈论的框架下探讨海洋渔业融资约束的形成与破解,根据现实情况将海洋渔业融资交易行为定为不完全信息动态博弈。研究结果表明:海洋渔业经营主体提供越高价值的抵押物,越易达成博弈的最优均衡,从而有效减少融资约束;金融机构越能准确识别海洋渔业经营主体生产投资活动的回报收益率,也越易达成博弈的最优均衡,从而有效减少融资约束。在此基础上,建议:扩大针对海洋渔业经营主体的融资抵押物范围,如海域使用权等用益物权可仿照土地经营权进行抵押试点;鼓励和引导设立相关担保机构和专项基金,从而在抵押物缺失的情况下支持海洋渔业经营主体的生产性融资;金融机构可尝试与海洋渔业经营主体建立长期的合作关系,从而降低双方的信息不对称程度,进而有效识别回报收益率,避免因潜在风险而产生的融资约束。     

基于Stokes-Helmert边值理论的大地水准面计算模型改化及分析检验

针对源自Stokes-Helmert边值理论的大地水准面计算模型适用性问题,首先详细解析了Stokes-Helmert方法的基本原理和计算模型,研究探讨了该方法与其他现有方法的关联性和差异性,分析比较了Stokes-Helmert计算模型和相同类型模型的技术特点,提出了Stokes-Helmert计算模型的实用改化方法,同时设计了4种分步改化模型的实验验证方案,使用超高阶位模型EGM2008作为数值模拟标准场,对分步改化模型的计算效果进行了数值精度检核,并开展了数据观测噪声影响评估检验,得出了一些有参考和实际应用价值的研究结论。在一定条件下,使用改化Stokes-Helmert方法计算(似)大地水准面可获得优于2cm的内符合度。     

基于AHP方法与GIS技术的海底管道路由选择研究

海底管道路由选择与海底管道建设、运营以及后期管理等工作存在密切联系,对管道工程经济性、安全性和合理性有着重要意义.考虑影响海底管道路由选择的自然与社会环境因素,构建了量化的评价体系,以AHP层次分析方法作为数学依据确定评价权重,建立了标准化的路由选择评判模型.进一步,将该模型与GIS空间分析技术相结合,生成以地图可视化...     

内蒙古北山地区阿民乌素公婆泉组变质火山岩年代学、地球化学特征及地质意义

内蒙古北山地区阿民乌素一带公婆泉组变质火山岩主要由钠长阳起岩、斜长阳起岩和斜长阳起片岩组成.三者主量元素显示相对高钠w(Na2O)=0.32％～2.46％,低钾w(K2O)=0.08％～0.38％、钛w(TiO2)=0.93％～1.03％,略富镁 w(MgO)=9.61％～12.04％、钙 w(CaO)=9.96％～1...     

Terrestrial heat flow and lithospheric thermal structure in the Chagan Depression of the Yingen-Ejinaqi Basin,north central China

The Chagan Depression in the Yingen-Ejinaqi Basin, located at the intersection of the Paleo-Asian Ocean and the Tethys Ocean domains is an important region to gain insights on terrestrial heat flow, lithospheric thermal structure and deep geodynamic processes. Here, we compute terrestrial heat flow values in the Chagan Depression using a large set of system steady-state temperature data from four representative wells and rock thermal conductivity. We also estimate the “thermal” lithospheric thickness, mantle heat flow, ratio of mantle heat flow to surface heat flow and Moho temperature to evaluate the regional tectonic framework and deep dynamics. The results show that the heat flow in the Chagan Depression ranges from 66.5 to 69.8 mW/m², with an average value of 68.3 ± 1.2 mW/m². The Chagan Depression is characterized by a thin “thermal” lithosphere, high mantle heat flow, and high Moho temperature, corresponding to the lithospheric thermal structure of “cold mantle and hot crust” type. We correlate the formation of the Yingen-Ejinaqi Basin to the Early Cretaceous and Cenozoic subduction of the western Pacific Plate and the Cenozoic multiple extrusions. Our results provide new insights into the thermal structure and dynamics of the lithospheric evolution in central China.     

Burial and exhumation of the Hoh Xil Basin,northern Tibetan Plateau: Constraints from detrital (U-Th)/He ages

The uplift and associated exhumation of the Tibetan Plateau has been widely considered a key control of Cenozoic global cooling. The south-central parts of this plateau experienced rapid exhumation during the Cretaceous–Palaeocene periods. When and how the northern part was exhumed, however, remains controversial. The Hoh Xil Basin (HXB) is the largest late Cretaceous–Cenozoic sedimentary basin in the northern part, and it preserves the archives of the exhumation history. We present detrital apatite and zircon (U-Th)/He data from late Cretaceous–Cenozoic sedimentary rocks of the western and eastern HXB. These data, combined with regional geological constraints and interpreted with inverse and forward model of sediment deposition and burial reheating, suggest that the occurrence of ca. 4–2.7 km and ca. 4–2.3 km of vertical exhumation initiated at ca. 30–25 Ma and 40–35 Ma in the eastern and western HXB respectively. The initial differential exhumation of the eastern HXB and the western HXB might be controlled by the oblique subduction of the Qaidam block beneath the HXB. The initial exhumation timing in the northern Tibetan Plateau is younger than that in the south-central parts. This reveals an episodic exhumation of the Tibetan Plateau compared to models of synchronous Miocene exhumation of the entire plateau and the early Eocene exhumation of the northern Tibetan Plateau shortly after the India–Asia collision. One possible mechanism to account for outward growth is crustal shortening. A simple model of uplift and exhumation would predict a maximum of 0.8 km of surface uplift after upper crustal shortening during 30–27 Ma, which is insufficient to explain the high elevations currently observed. One way to increase elevation without changing exhumation rates and to decouple uplift from upper crustal shortening is through the combined effects of continental subduction, mantle lithosphere removal and magmatic inflation.     

城市内涝灾害受灾人口评估方法与实证研究：以哈尔滨市道里区为例

城市内涝灾害频发,对居民生命安全造成严重威胁,为提高城市内涝灾害受灾人口评估精度,提出一种更为精确的受灾人口评估方法。以哈尔滨市道里区为研究区,以城市内涝灾害受灾人口为研究对象,运用一、二维非恒定流为主控方程,构建城市内涝数值模拟模型,并结合受灾人口分布特点,综合构建基于土地利用的人口随时间变化的计算模型。实现在模拟内涝灾害影响范围基础上,利用受灾人口计算模型提取白天与夜晚受灾人口分布情况。结果表明：研究区在百年一遇降雨情景下,有25条街道会发生不同程度积水,积水深度范围值为0.10~1.42 m;此级别内涝灾害在白天11条街道受灾人口数量最大值达到3 500人,夜晚10条街道受灾人口数量最大值为720人。     

Building national eco-cultural protection areas and the Xiangxi practice in Hunan Province

Journal of Geographical Sciences - Since 2007, the Chinese government has initiated the building of national eco-cultural protection areas (NECPAs), thereby embarking on a significant...