Coastline configuration and geomorphologic development mode of arc-shaped coast in South China

Coastline configuration indexes of 34 typical arc-shaped coasts in South China are investigated by the method of principal component analysis, and meanwhile deposition and geomorphologic features of arc-shaped coast are also analyzed. The results show: (1) The configuration of arc-shaped coast in South China is of the characteristic of variability and complexity. (2) The wave power and the openings of the bay are the decisive factors to result in the changes of the configuration of the arc-shaped coast in South China, however, incidence direction of the wave has no effect on configuration development of the coast. (3) Commonly, geomorphologic modes of the arc-shaped coast system in South China consist of barriers, lagoons and tidal-inlets, and can be divided into four types:the openings of the bay leaning to the east, the openings of the bay leaning to the south, the openings of the bay leaning to the west and the openings of the bay leaning to the north.

Coastal dune rock development and Holocene climate changes in South China

Coastal dune rocks in China are eolian sands cemented by calcium carbonate under subaerial conditions, widely distributing on the tropical and subtropical coasts of South China. Particular temperature and precipitation as well as local wave and landform conditions are required for the formation of the dune rocks. A correspondence was found between Holocene environmental changes and coastal dune rock development by comparing the features of the sea-level and climate changes in the Holocene period with the ages, scales, and cementation of the dune rocks on the South China coasts. The findings provide well grounded explanation for some problems unresolved in the past researches on the coastal dune rock in South China： （1） There were no dune rocks with ages older than 6000 years in South China because the dune rocks formed before 6000 a BP were covered by the sea water that rose in the later period; （2） the dune rocks with ages of around 3000 a BP were widely found in South China today because the coastal dunes were cumulated on a large scale at that time as a result of temperature falling after the end of Megathermal; （3） Medieval Warm Period was the main period for the eolian dunes to be cemented into the coastal dune rocks in South China; （4） lack of dune rocks of younger than 1000 a BP was accounted for by that the climate conditions in recent one thousand years were not suitable for the cementation.

Analysis of wave shoaling and shore-breakers on a low tide terrace beach based on in-situ measurements at Xisha Bay on South China coast

Low tide terrace beach is a main beach type along South China coasts with strong tidal actions.How strong tides affect wave transformations on low tide terrace beach still remains unclear.In this study,in-situ measurements are conducted on the low terrace beach at Xisha Bay to provide quantitative descriptions of wave shoaling and shore-breaker phenomena under the tidal effects.It is found that wave breaking is unsaturated on the low tide terrace beach at Xisha Bay.Magnitudes of wave skewness and asymmetry increase as wave shoals and achieve the maximum value at the shore-breaker,and then decrease rapidly.Mean energy dissipation rates of shore-breakers are tide-modulated since the bottom slope changes at the shoreward boundary of wave propagation in a tidal cycle.The remaining wave energy flux at the initialization of the shore-breaker is 1%–12%of offshore wave energy flux,and the energy flux ratio decreases with increasing offshore wave heights.Wave attenuation at shore-breakers can be estimated directly from offshore wave conditions based on findings in this study,favoring designs of seawalls or beach nourishment projects.Field datasets on wave transformations can also be used for verifications of wave numerical models.

Thermodynamics and Microphysical Characteristics of an Extreme Rainfall Event Under the Influence of a Low-level Jet over the South China Coast

In this paper,the data of Automatic Weather Stations(AWSs),ERA5 reanalysis,sounding,wind profile radar,and dual-polarization radar are used to study an extreme rainfall event in the south China Coast on 11 to 12 May 2022 from the aspects of thermodynamics and microphysical characteristics under the influence of low-level jets(LLJs).Results show that:(1)The extreme rainfall event can be divided into two stages:the first stage(S1)from 0000 to 0600 LST on May 12 and the second stage(S2)from 0700 to 1700 LST on the same day.During S1,the rainfall is mainly caused by the upper-level shortwave trough and the boundary layer jet(BLJ),characterized by strong upward motion on the windward side of mountains.In S2,the combined influence of the BLJ and synoptic-system-related low-level jet(SLLJ)increases the vertical wind shear and vertical vorticity,strengthening the rainstorm.In combination with the effect of topography,a warm and humid southwest flow continuously transports water vapor to farther north,resulting in a significant increase in rainfall over the study area(on the terrain’s windward slope).From S1 to S2,the altitude of a divergence center in the upper air decreases obviously.(2)The rainfalls in the two stages are both associated with the mesoscale convergence line(MCL)on the surface,and the wind field from the mesoscale outflow boundary(MOB)in S1 is in the same direction as the environmental winds.Due to a small area of convergence that is left behind the MOB,convection moves eastward quickly and causes a short duration of heavy rainfall.In S2,the convergence along the MOB is enhanced,which strengthens the rainfall and leads to strong outflows,further enhancing the surface convergence near the MOB and forming a positive feedback mechanism.It results in a slow motion of convection and a long duration of heavy rainfall.(3)In terms of microphysics,the center of a strong echo in S1 is higher than in S2.The warm-rain process of the oceanic type characterizes both stages,but the convective intensity in S2 is significantly stronger than that in S1,featuring bigger drop sizes and lower concentrations.It is mainly due to the strengthening of LLJs,which makes small cloud droplets lift to melting levels,enhancing the ice phase process(riming process),producing large amounts of graupel particles and enhancing the melting and collision processes as they fall,resulting in the increase of liquid water content(LWC)and the formation of large raindrops near the surface.

Preliminary research on sea-level changes of the South China coast since late Epipleistocene

Several views on sea-level changes of the South China coast are briefly introduced in this paper. On the basis of 236 samples whose ages are determined by 14C chronological method and their sites are corrected with ancient water depth and crustal deformation, a basic model about sea-level changes of the South China coast since late Epipleistocene is set up. This model basically accords with the general cognitions of predecessors, i. e. it not only represents the common characteristics of sea-level changes of the East China coast but has some features of the South China coast itself. In general, this model is relatively close to the Fairbridge's curve, indicating that the sea-level undulations exist since 6 ka ago but the ranges of undulations are slightly larger than those of Fairbridge's curve.

A study on Holocene aeolian shell-clastic sandstonesalong the coasts of South China andthe analysis of its formation

The Holocene aeolian shell-clastic sandstones at 13 places along the coasts of Fujian, Guangdong and Hainan Provinces are studied in the following respects; describing their features from both macroscopic and microscopic views, listing their distributions, altitudes and forming ages, and discussing the nomenclatures of this kind of rock and its differences from beach rock.

Temperature variability caused by internal tides in the coastal waters of east coast of Peninsular Malaysia

The effects of tidal currents(i.e., barotropic and internal tides) are important in the biogeochemistry of a coastal shelf sea. The high-frequency of currents and near-bottom temperatures collected in three consecutive southwest monsoon seasons(May, June, July and August of 2013 until 2015) is presented to reveal the role of the tidal currents to the temperature variability in the coastal shelf sea of the east coast of Peninsular Malaysia(ECPM),south of the South China Sea(SCS). The results of a spectral density and harmonic analysis demonstrate that the near-bottom temperature variability and the tidal currents are influenced by diurnal(O_1 and K_1) and semidiurnal(M_2) tidal currents. The spectral density of residual currents(detided data) at 5, 10 and 16 m depth also shows significant peaks at the diurnal tidal frequency(K_1) and small peaks at the semidiurnal tidal frequency(M_2)indicating the existence of internal tides. The result of the horizontal kinetic energy(HKE) shows a strong intermittent energy of internal tides in the ECPM with the strongest energy is found at 16 m depth during a sporadic cooling event in June and July. A high horizontal cross-shore heat flux(16 m) also indicates strong intrusions of cooler water into the ECPM in June and July. During the short duration of cold pulse water observed in June and July, a cross-wavelet analysis also reveals the strong relationship between the near-bottom temperatures and the internal tidal currents at the diurnal tidal frequency. The intrusion of this cooler water is probably related to the monsoon-induced upwelling in June. It is loosely interpreted that the interaction between the strong barotropic tides and the steep slope in the central basin of the SCS under the stratified condition in southwest monsoon has generated these internal tides. The dissipation of internal tides from the slope area probably has driven the cold-upwelled water into the ECPM coastal shelf sea when the upwelling intensity is the highest in June and July.

华南地区地震热异常变化特征分析

利用数据库2006年以来的卫星热红外亮温资料,统计并研究华南沿海5级及海南邻近区域4级以上地震。研究结果表明:64.7%的地震在震前存在明显的热红外异常异常总体特征为出现—增加—极大值—减弱—消亡的过程,不同地震出现异常的对应周期不同,主要以第一对应周期为主,地震大多发生在异常达到峰值后两个月内。异常的最大幅值与震级没有正相关的关系,可能与震前几年是否出现过高值异常有关,是个相对值。

海洋空间的“领土化”构建与实践 ——以美国在南海地区的干涉行动为例

随着海洋与人类的联系越来越密切,控制人类海上活动的必要性,令海洋空间的“领土化”成为难以避免的趋势。主流话语开始从将海洋描述为无主之地,变成倾向于为扩大公共权力对海域控制的做法辩护,为海上力量投送和海域管控编织正当理由。由此,产生了一定的海洋空间“领土化”,国家从规范功能的角度逐渐控制海洋空间,将公共权力投射至领海和管辖水域外的海域。塑造符合自身利益需求的地区规范秩序,并在实践上强化地区军事力量投送,这两种海洋空间“领土化”扩张方式,鲜明地体现在美国在南海地区的干涉行动中。中国需在南海促进建设更有效的海洋治理体系,扩大行为规范塑造和海洋新秩序建设上的话语权,更好地维护国家海洋安全和发展利益。

北极海空搜救合作模式对建构南海搜救合作体系的借鉴与启示

南海作为重要的国际运输通道,面临日益增长的多元化海上安全威胁,搜救合作的制度化建构进程日益紧迫。北极海空搜救已经形成较为成熟的搜救合作机制,与其他半闭海水域海空搜救合作机制相比较,北极搜救模式经验借鉴更适用于南海。南海沿岸国需要考虑在“南海行为准则”磋商中加入区域性指导规范以夯实南海搜救合作法律基础,建立“南海合作理事会”以强化机构管理,建构海上搜救基金协同机制以保证基金供给稳定,辩证看待域外国家搜救参与以加强搜救效果。中国应当主动贡献中国力量,在搜救合作制度化建设中发挥南海区域大国的主导性作用。

华南砂质海滩的动力地貌分析

为探讨华南砂质海滩的动力地貌学特征,对不同地理岸段不同地貌形态的8 个沙滩剖面于冬、夏季进行现场重复调查和室内分析工作.据此,通过对华南海岸带地质构造、地貌和现代海岸动力环境地域变化的分析,将华南沿海砂质海岸划分为岬湾岸、沙坝潟湖岸和夷直岸三种基本海岸地貌类型,并且从滩面倾向、海岸动力环境影响、季节冲淤变化趋势和滩面沉积物粒径、坡度的动力响应等方面探讨砂质海滩的动力地貌,得出其受制于多种环境因素的影响,其中地质构造背景和海平面变化为大尺度的砂质海岸地貌的发育奠定了基础,而全新世海侵海平面相对稳定后,海岸动力条件的塑造起着决定性的影响,浪潮作用指数是其中重要的影响指标.

红树林生长带与潮汐水位关系的研究

根据海南东寨港林市村、廉江车扳镇那腮村、深圳锦绣中华等3个实验点10条横断面红树林潮滩高程水准测量，林市村潮汐水位观测，潮汐特征水位及浸淹频率分布计算，参照有关港点潮汐实例或预报资料，确定红树林外边界为平均海面或稍上，内边界（或林内最大高程）为回归期平均高高潮位（或大潮平均高潮位）。对国内外有关报道进行了评述。指出国内许多红树林文献中使用的“高潮位”、“中潮位”、“低潮位”用潮汐学术语表述应为“回归潮（或大潮）高潮位”、“中期高潮位”、“分点期（或小潮）高潮位”。明确红树林生长带位于平均海面以上的潮滩，对红树林建立和演替的研究，红树林宜林地选择及用红树林泥炭研究海平面变化均有重要意义。

2000年来华南沿海气候与环境变化

通过华南沿海两个钻孔剖面的孢粉分析，并用14种热带、南亚热带木本植物花粉含量之和与5种中、北亚热带和暖温带木本植物花粉含量之和的比值作为冷热变化的温度半定量曲线；利用2000年来古籍、地方志记载的典型热带动、植物分布、兴衰的变化作冷暖变化事件；以华南沿海罕见的降雪记载，特别是对15世纪以来的降雪现象分纬度统计其出现频率，探讨华南的小冰期。据此分析华南沿海2000年来的气候和环境变化。

南海北部陆区岩石磁化率的矿物学研究

基于2517套现场测量资料，245块岩石样品的体积磁化率测量和详细的岩矿鉴定及硅酸盐全分析结果，结合单矿物磁化率特征及各岩石之间的对比研究，发现岩石磁化率主要受组成岩石的矿物磁化率控制．即岩石磁化率（峰）与组成岩石各个矿物磁化率（峰）及其体积含量（G）成正比．例如侵入岩磁化率，kr=-5．68×10^2Cq＋2．86×10^2C1＋3．28×10^2Ca＋1．18×10^4Cb＋1．27×10^4Cam＋5．35×10^5Cm；其中多项式各项的系数是与该矿物磁化率值成正比的常数，C为该矿物在该岩石中的体积含量，依次为石英q（k=-1.3）、斜长石f（k=0．01）、碱性长石a（k=0．01）、黑云母b（k=100）、角闪石am（k=80）和磁铁矿m（k=100000）．对区内火山岩、侵入岩、沉积岩和变质岩磁化率研究发现，其他三类岩石磁化率与其组成矿物磁化率的关系和侵入岩的情况相同，矿物对岩石磁化率的贡献顺序为铁磁性矿物〉顺磁性矿物〉逆磁性矿物．其中，火成岩磁化率变化大，主要取决于岩石中磁铁矿、角闪石和黑云母的含量；沉积岩多为无磁性、弱磁性，其磁化率主要由黑云母、碱性长石及岩屑提供；变质岩的磁性变化较大，从无磁性到极强磁性，主要决定于其原岩的类型，副变质岩（沉积原岩）磁化率类似于沉积岩类，正变质岩（火成原岩）类似于火成岩类；石英岩和碳酸盐岩是所有岩石中磁性最弱的．岩石蚀变会对其磁化率产生显著性影响，通常，黑云母、角闪石等铁镁硅酸盐矿物经蚀变会因形成含铁质氧化物而使岩石的磁化率升高；长石等弱顺磁矿物的粘土矿化、绢云母化会升高磁化率而碳酸盐化、高岭土化作用会使磁化率降低；岩石的绿泥石化会增加磁化率；含铁磁性矿物的岩石风化时会因高磁性组分破碎、流失而致使岩石的磁化率降低．从岩石磁化率与其组成矿物的磁化率之间的关系，推测地质体的总磁化率与构成地质体各个岩石的磁化率一体积含量之间也应存在类似关系．

华南沿海牡蛎重金属含量特征及其风险评估

根据2009年对华南沿海部分海域的近江牡蛎和太平洋牡蛎的监测数据,对产品中重金属元素Cd、Cu、Pb、As、Hg和Zn的含量水平、分布与变化特征进行了分析讨论;采用点评估方法,计算Cd、Cu、Pb、As、Hg和Zn的膳食暴露量,对牡蛎产品的食用安全性进行风险评估。结果表明,调查海域牡蛎样品中Cu、Zn、Cd的含量较高,其值分别为92.0、268、1.32 mg/kg(湿重,下同);Hg、As、Pb的含量低,其值分别为9.21、0.11、0.26 mg/kg。不同海域、不同养殖季节的牡蛎产品中重金属元素的含量具有明显的差异。与无公害水产品质量标准的限量值相比,调查海域牡蛎产品中Cu、Zn、Pb、Hg、As的含量符合产品质量标准,Cd的含量超过产品限量标准值。由于元素间的相互作用,牡蛎产品Zn的含量高、Cd的含量低,Zn的可利用性阻止对Cd的吸收,牡蛎产品中的Cd不会对健康造成危害。风险评估的结果显示,每周食用适量的牡蛎,重金属的膳食摄入量低于世界卫生组织/联合国粮食和农业组织的食品添加剂联合专家委员会(JECFA)推荐的暂定每周耐受摄入量,处于安全范围内。

华南沿海温泉成因探讨

首先分析了华南沿海温泉成因 ,排除该区多数温泉具局部衰变热、岩浆残余热、断层活动热成因的可能性。重点讨论了地下水深特循环的动力学模型 ,分析了地下水循环深度 (相当于张性断层的规模 )和水头压力(相当于地形反差 )对泉温和流量的控制作用 ,并把泉温和流量与理论计算曲线对比 ,从而得出华南温泉为深循环的成因的结论。分析还得出 ,较大地形反差和张性大断裂是温泉形成的两个有利条件 ,如果仅具备其中一个条件 ,那么张性大断裂 (小地形反差 )比大地形反差 (小断裂 )更有利于获得较高泉温。可见 ,温泉深循环的动力学模型对华南沿海地热资源的预测、开发和利用有一定的指导意义。最后 。

华南红树林海岸生物地貌过程研究

红树林生物地貌过程是全球变化海岸带陆海相互作用研究重点内容之一。本文以海南东寨港林市村,广东廉江高桥镇凤地村和车板镇那腮村以及广东深圳福田和锦绣中华3个半定位试验区有关红树林群落结构、潮汐动力、沉积特征和地貌特征的调查资料为基础,探讨红树林生物地貌过程的生物学基础,沉积地貌表现,红树林生态系对人类活动和海平面上升的响应。

南海北部沿岸贝类体内镉含量及健康风险评价

根据2007年和2009年对南海北部沿岸菲律宾蛤仔(Ruditapes Philippinarum)、翡翠贻贝(Perna viridis)、近江牡蛎(Crassostrea rivularis)、太平洋牡蛎(Crassostrea gigas)、文蛤(Meretrix meretrix)5种贝类的监测资料,对贝类体内Cd的含量水平进行了分析讨论;采用点估计的方法,评估贝类Cd的暴露量,对其安全性进行评价。结果表明,调查海域近江牡蛎、太平洋牡蛎、菲律宾蛤仔、翡翠贻贝和文蛤样品中Cd的平均含量分别为:1.80、0.38、0.12、0.26和0.15 mg.kg-1,其变化范围分别为:0.92～2.39 mg.kg-1、0.31～0.46 mg.kg-1、0.10～0.13 mg.kg-1、0.21～0.30 mg.kg-1和0.08～0.22 mg.kg-1。与其他海域贝类调查的数据相比,此次调查贝类体内Cd含量处于正常的波动范围。风险评估结果显示,近江牡蛎的风险商HQ>1,表明人体存在过量摄入Cd的风险;其他4种贝类的HQ<1,处于安全范围内。评价结果还显示,儿童的Cd暴露量高于成年人。此次调查近江牡蛎样品中Cd/Zn的比值(0.005)低于0.015的临界值,从微量元素平衡的角度,近江牡蛎中Cd的健康风险低。

华南沿海若干砂质海滩沉积物粒度特征的分析

根据2003年7月在华南沿海12个砂质海滩所取得的76个沉积物样品(其中次表层样品36个,不计入研究范围),就该区的沉积物粒度特征展开论述。为了便于分析其沉积物粒度特征,我们把华南沿海12条海滩剖面根据岸滩形态和成因将华南砂质海岸划分为岬湾型砂质海岸、沙坝-潟湖型砂质海岸和夷直型砂质海岸三大类。阐述了不同类型海滩的表层沉积物的粒度特征、类型、分布以及粒度的沿程变化特征。