未来海岸环境变化的易损范围及评估--江苏滨海平原个例研究

以海面上升与灾害加剧为标志的海岸环境变化将是２１世纪海岸地区社会经济发展面监 的最严峻挑战。评估未来海岸环境变化的易损性是联合国政府间气候变化专门委员会（ＩＰＣＣ）敦促沿海各国政论在评估气候变化及其影响是必须先优开展的工作之一。针对已有在研究存在的问题,发展了适用于面积广阔、微地貌条件复杂且有海堤保护的大河三角洲和滨海平原海岸环境变化易损范围确定和易损性评估的方法。并基于江苏滨海平原黄型潮滩剖面外     

Analysis on water supply and demand of North China Plain

IntroductionIn terms of water resources supply and demand analysis, the North China Plan which is the main waterreceiving area of the proposed southjnorth water transfer project, is often considered as a whole region.Adrinistrahvely, the region includes mbocipalihes of Beding and Tianjin, most pal'ts of provinces ofHebei (herealler known as Hebei), Henan olereafter known as Henan) and Shandong (herealler known asShandong) able l). The Nortll China Plain covers an area of 191 250 klllZ wi…     

松嫩平原西部盐沼的形成与演化

本文运用环境变迁的理论和方法,较系统地分析了松嫩平原西部盐沼的形成与演变机制。本区沼泽形成的主要控制因素是古河道变迁、新构造运动、风力作用、古气候变化。沼泽残余盐碱化与晚更新世松辽大湖的消亡、河道变迁有关,现代盐碱化则主要是水利工程、植被破坏和气候变化引起的,而且呈迅速加剧的趋势。防治沼泽盐碱化的主要措施是实施水稻和芦苇开发、大规律建立蓄洪区和自然保护区。     

三江平原大面积开荒对自然环境影响及区域生态环境保护

根据多年在三江平原野外考察积累的大量资料,对比开垦前后不同年代的数据,分析在江平原大面积开荒引起的区域环境变化,包括生态类型的变化,土地退化、水环境变化以及动植物资源的变化等,并在总结三江平原开荒过程中经验教训的基础上提出区域环境保护对策。     

黄淮海平原沙区发展农业产业化初步研究——以河南省延津县为例

农业产业化是一种新兴的农业经济发展模式,在黄淮海平原沙区尚属起步阶段。通过对河南省延津县沙区基本条件的分析研究,结合黄淮海平原沙区发展两高一优及可持续农业的可行性,对延津县沙区发展农业产业化进行了探讨,提出了以发展林果、畜牧和种植业等3大支柱产业为主的农业产业化生产体系,以期对黄淮海平原沙区农业的发展起到促进作用。     

河北平原地下水4He年龄初探——以满城-任丘剖面为例

以满城-任丘剖面为例,采用过剩空气非分馏(UA)模型进行了单独He成分的分离,第三含水组中含有的过剩4He是含水组(Q2)内原地产量和地壳通量的综合结果.由于缺乏确定He平衡参数的约束条件,选择了应用地下水流模型主观调节来估算迭代过程中外部通量和流速场,然后根据这个模型所取得的4He年龄与应用其他方法包括14C测年和水文模型取得的年龄作对比,取得了河北平原第三含水组满城-任丘地下水的4He年龄为0～30 ka的结果.     

汾渭平原一次沙尘和人为混合空气污染过程分析

利用MODIS、OMI和CALIPSO卫星资料,结合地面环境监测数据、气象观测数据和后向轨迹模式(Hybrid Single Particle Lagrangian Integrated Trajectory Model,HYSPLIT),对汾渭平原2018年11月23日至12月6日沙尘和人为混合空气污染过程进行分析....     

围垦对鄱阳湖洪水位的影响及防治对策

１９９２年１０月,在江汉平原沔城钻探,取得总长５６．１８ｍ的柱状岩芯。根据Ｍ１孔湖泊沉积岩性及所含文化遗物,＾１４Ｃ年代测定,以及深受人类活动影响的气候与环境指标如孢粉,频率磁化率,化学元素Ｐ等分析,结合该区文化遗址的时空分布,揭示了沔城地区中晚全新世人类活动的时间序列及与古气候,古环境的关系：６．７－３．５ｋａＢＰ该区气候温暖湿润,为河间洼地和浅湖环境;２．５－１．７ｋａＢＰ湖泊稳定,均无人类居     

流域数据模型研究—以太湖流域西苕溪流域为例

对江汉平原江陵剖面沉积物中的总有机碳（TOC）、总氮（TN）、有机碳同位素δ13C值和粒度参数的分布特征与环境气候的关系进行了研究.结果表明：沉积物中有机碳、总氮较高,有机质的δ13C值偏负,沉积物的平均粒径较粗时,气候温暖湿润;反之,沉积物中有机碳、总氮较低,有机质的δ13C值偏正,沉积物的平均粒径较细时,气候温凉偏干.结合14C测年,判别江汉平原江陵地区的古气候演化过程：8900-6070 aBP,为温湿时期;6000-4600 aBP为相对冷干时期;4600-2500 aBP为温暖湿润时期;2500 aBP以来为温凉偏干时期.     

Determination of sediment volumes, accumulation rates and turbidite emplacement frequencies on the Madeira Abyssal Plain (NE Atlantic): a correlation between seismic and borehole data

The sedimentary infill history of the Madeira Abyssal Plain (MAP) is established from correlation of ODP Leg 157 drillsites (Sites 950–952) with an almost regular grid of 7000 km of intermediate-resolution seismic reflection profiles covering the central part of the abyssal plain. The most conspicuous seismic reflectors bounding the seismostratigraphic units have been identified and mapped. Correlation between seismic and borehole data using synthetic seismograms allows the lithological attribution and dating of the reflectors and seismostratigraphic units. Lateral mapping and correlation of seismic units also allows both the volumes and rates of accumulation of sediments within each seismostratigraphic unit and equivalent time periods of deposition to be determined. These calculations have been corrected for the effect of compaction, calculated at around 40% at the base of the drillholes. Three main turbidite types have been identified at the drillsites and their emplacement frequency has been calculated for each site and time period. Our results show that Cretaceous oceanic crust was draped with red pelagic clays, and the fracture-zone valleys were completely infilled and levelled in a geologically rather short time, probably during the latest Oligocene and Early Miocene, by organic-rich turbidites derived from the NW African continental margin. At 16 Ma, the topography was levelled enough to allow large turbidity current flows to cover the entire plain. During the Middle and Late Miocene (16–5.9 Ma), organic-rich turbidites were emplaced on the abyssal plain at a low rate of accumulation (12 m/my). In the uppermost Miocene–Early Pliocene (5.9–3.6 Ma), turbidite emplacement increased markedly in both frequency and accumulation rate (e.g., 26 m/my for organic-rich turbidites). During this time, period emplacement of volcanic-rich turbidites also increased in volume and frequency, a trend that continued into the Pliocene. Increased volcanic-rich turbidite emplacement correlates well with increased volcanic activity on the Canary Islands, and increased organic-rich turbidite emplacement may correlate with periods of erosion on the NW African continental margin. These erosional periods may be related to global cooling and falling sea level, intensification of bottom-water currents, and enhanced upwelling on the margin.