南海北部陆坡ZSQD196PC柱状样末次间冰期以来的古海洋学记录：氧同位素、有孔虫和硅藻     

李顺  张江勇  钟和贤  高红芳  陈炽新  庄畅 《海洋地质前沿》2013,(11):32-38

为了解南海北部陆坡末次间冰期以来的古海洋沉积环境演化特征,对研究区ZSQD196PC柱状样有孔虫、硅藻及有孔虫氧同位素资料开展了分析。依据沉积有孔虫、硅藻主要属种的百分含量、丰度及组合特征,将有孔虫划分为3个组合,分别对应于氧同位素MIS1、2、3~4期;将硅藻划分为4个组合,大致对应于MIS1~4期。MIS1期有孔虫以暖水种占优势,Pulleniatina obliquiloculata百分含量显著升高;硅藻丰度低且以热性种占优势,其中冷期出现大量沿岸种,反映相对温暖的气候条件。MIS2~4期有孔虫以冷水种占优势,温跃层种含量相对较高;硅藻丰度高且以广布种占优势,出现沿岸种含量的升高,反映较冷的气候条件。通过对比浮游有孔虫氧同位素,分析讨论了末次盛冰期、Blling—Allerd暖期和新仙女木事件在ZSQD196PC柱状样的沉积响应,揭示了末次冰期中的气候波动。  相似文献   

基于IHS的多源遥感数据融合     

廖文峰 《地理空间信息》2012,(1):99-101,4

首先简要叙述了IHS法在遥感图像融合中的应用,然后对实验结果进行了分析,并用融合后的图像建立了土地利用类型的解译标志,以期为HIS法用于遥感图像融合提供参考。  相似文献   

朝阳市水资源监测分析与展望     

李和  王伟  赵福明 《地下水》2009,31(3):36-37,47

针对朝阳市水资源短缺、水污染加重的实际状况,从如何管好、用好有限的水资源实现水资源可持续利用的战略高度,深入分析了"十一·五"前全市水资源监测、研究、服务的发展过程,揭示了当前水资源监测、分析工作中存在的实际问题,系统地论述了水资源监测分析对水资源配置、管理、保护、研究的作用及重要性,阐明了"十一·五"期间全市水资源监测分析的发展方向及奋斗目标.  相似文献   

亚热带马尼拉草坪生态系统CO_2净交换量测定方法比较     

李熙波  杨玉盛  曾宏达  谢锦升  张静  朱宁 《福建地理》2008,(4)

利用IRGA法和GC法,同步观测了3种天气(晴天、多云、阴天)条件下福州市江滨公园马尼拉草坪生态系统CO2净交换量(NEE)的白昼动态变化,比较IRGA法和GC法透明通量箱对观测样点环境的影响程度,并探讨其对NEE观测结果的影响.结果表明:在单次观测结束时,IRGA法通量箱对样点环境的扰动小于GC法,晴天白天二者箱内的平均升温分别为1.79℃和2.33℃,箱内平均光合有效辐射(PAR)降低幅度分别为11.00%和21.00%.3种天气情况下,IRGA法与GC法观测的NEE白天变化趋势较一致,但3种天气相同时段内GC法测定的NEE平均值比IRGA法高3.17μmol·m-2·s-1,二者的差异在中午最大,在清晨和傍晚较小.IRGA法比GC法可以更为准确地测量草坪NEE.  相似文献   

Sinohyliopsis schlegeli珍珠层中Si、Mn、Fe和Sr离子的微生物固定化和环境因素     

Kazue Tazaki Issei Morii 《地学前缘》2008,15(6):54-65

在日本Ishikawa Prefecture的Kanazawa大学进行了为期8个月的排水池培养实验,利用特征水和营养元素的基本因素对Sinohyliopsis schlegeli贝壳珍珠质所记录的环境变化进行观察。在2007年5月份到11月份之间,每个月向贝壳珍珠质注入四环素作为指示剂。定期测量水质,诸如pH、氧化还原势、电导率、溶解氧以及水温,通过过滤法除掉水中悬浮固体并进行光学显微镜和荧光X射线分析以及扫描电镜 能量色散X射线观察(SEM EDX)。对贝壳珍珠质的X射线荧光化学分析表明那些富含四环素的层对应高含量的Si、Mn、Fe和Sr离子。氧化还原势和溶解氧分析都证明在珍珠质中存在层。排水池中悬浮物质主要由Si、Mn和Fe元素组成,这与2007年夏季贝壳珍珠层的生物固定化中所涉及的元素一致。SEM EDX分析证明离子来自Siderocapsa sp.和Gallionella ferruginea硅藻的胃部。冬季几乎没有发生离子的生物固定化。结果表明在层化的贝壳珍珠质中存在元素的固定化,Sinohyliopsis schlegeli 在夏季以离子为食来生长珍珠质。具有这些生物氧化物的Sinohyliopsis schlegeli可能对自然界水体中重金属的清除有一定的贡献。  相似文献   

Late Quaternary diatom and sea level changes in estuarine plain of the Jiulong River     

Chen Wenrui  Lan Dongzhao  Chen Chenghui 《海洋学报(英文版)》1998,17(4):509-518

TheJiulongRiver,composedoftheWestStream,theNorthStreamandtheSouthStream(seeFig.1)isthesecondlargestriverinFujianProvince.ItsestuarineplainintervenesbetweenthetwqcitiesofXiamenandZhangzhou,withsouthern-subtropicoceanicmonsoonclimate-SofartherehasnotbeensystematicresearchontheLateQuaternarysea1evelchangesinthearea,andthispaperisintendedtodosomethingaboutit.DIAToMZoNESANDBIoFACIESOFZK5BoREHOLETheBoreholeZK5islocatedtothenortheastofHaichengTown,withcoordinateof24"24,32*N,ll7'5…  相似文献   

Redeposition of volcaniclastic sediments by a tsunami 4600 years ago at Kushima City,south-eastern Kyushu,Japan     

Masaki Yamada  Shigehiro Fujino  Takashi Chiba  Kazuhisa Goto  James Goff 《Sedimentology》2020,67(3):1354-1372

The Hyuga-nada Sea, south-eastern Kyushu, Japan, is located between a strong (Nankai Trough) and a weak interplate coupling zone (Ryukyu Trench). Over the past 400 years this area has only experienced Magnitude 7·5 earthquakes or smaller and associated small-scale tsunamis. However, this short historical record most likely does not include the full range of high magnitude, low frequency giant earthquakes that might have occurred in the region. Thus, it is still unclear whether giant earthquakes and their associated tsunamis have occurred in this region. This paper reports on a prehistoric tsunami deposit discovered in a coastal lowland in south-eastern Kyushu facing the Hyuga-nada Sea. There is a reddish-brown pumiceous layer preserved in a non-marine, organic-rich mud sequence obtained from onshore sediment cores. This layer is recognized as the ca 4600 year old Kirishima-Miike tephra (that is now placed around 4500 years ago) sourced from Mount Kirishima, southern Kyushu. Another whitish pumiceous layer is evident below the Kirishima-Miike tephra in almost all of the sediment cores. A relatively high percentage of marine and brackish diatoms is recorded within this lower pumiceous layer (but not in the surrounding muds or in the overlying Kirishima-Miike tephra), indicating a marine or beach sediment source. Plant material obtained from organic-rich mud immediately below the event layer was dated to ca 4430 to 4710 cal yr bp , providing a limiting-maximum age for this marine incursion event. The presence of marine diatoms below the event layer is probably explained by pre-seismic subsidence. An absence of the resting spore of the planktonic brackish diatom Cheatoceros and the appearance of the freshwater diatom Eunotia serra immediately above the event layer probably represents a marked change to a relatively low-salinity environment. Assuming that there were no significant local geomorphological changes, such as drainage obstruction caused by formation of a new barrier spit, it is considered that co-seismic or immediate post-seismic uplift are the most likely explanations for this notable environmental change. Based on the crustal movements noted before and after the marine incursion, this event is interpreted here as an earthquake-generated tsunami. Moreover, because of these notable seismic crustal movements the tsunamigenic earthquake probably occurred immediately offshore of the study site.  相似文献   

南黄海生物硅的时空变化     

张丹  鉴珊  孙军  冷晓云  张桂成 《海洋学报(英文版)》2019,38(12):101-110

Concentrations of biogenic silica(BSi) in the southern Yellow Sea were determined during four cruises(spring:April–May 2014; autumn: November 2014; summer: August–September 2015; winter: January 2016). Samples of BSi were measured using the double extraction method. Seasonal and spatial variations of BSi and the potential correlation between chlorophyll a(Chl a) content and BSi in four seasons were measured in this study. Significant spatial variability was observed in seawater BSi concentrations. The average concentration of BSi was highest in winter and lowest in spring. Furthermore, the relationships between concentrations of BSi and hydrological parameters were also discussed. There was a significant positive correlation between Chl a and BSi. The concentrations of BSi showed significant relationships with temperature and the concentrations of silicates, total inorganic nitrogen and total inorganic phosphorus, indicating that distribution of BSi was affected by temperature and nutrient level.  相似文献   

多胺对3株硅藻生长的影响          下载免费PDF全文

赖雯奕  娄亚敏  徐继林  周成旭  严小军 《海洋学研究》2018,36(3):96-100

为探究多胺对硅藻生长的影响,以精胺、亚精胺、腐胺、尸胺和苯乙胺为外源多胺,对角毛藻Chaetoceros sp.、小新月菱形藻Phaeodactylum tricornutum Bohlin以及威氏海链藻Conticribra weissflogii进行室内添加培养。结果表明:同一温度下,不同多胺对不同硅藻生长存在特异性差异。亚精胺对角毛藻的生长起促进作用;尸胺对小新月菱形藻起促生长作用,而精胺对小新月菱形藻起抑生长作用;多胺对威氏海链藻生长前期(13 d前)主要起促生长作用,后期起抑生长作用(13 d后)。因此,适时适量添加多胺可有效促进硅藻的生长,提高硅藻的繁殖效率。  相似文献   

广州港新沙港区板桩码头结构设计方案比选分析     

刘洪超  李华 《海岸工程》2020,39(1):53-59

介绍了广州港新沙港区板桩码头主要内力计算方法及常用软件,结合设计过程、工程地质情况、现场实际施工情况,着重从受力合理性、施工便利性、节省造价方面,对提出的钢板桩方案、钢管板桩方案进行比较分析,确定了钢管板桩结构更合理,并对优势进行总结。研究表明相对于钢板桩结构,钢管板桩结构在抗弯、抗变形、拉杆拉力和锚碇墙稳定性、对复杂地基(软弱土层较厚、岩层标高较高的地基)适应性、兼顾桩基基础、施工速度等方面更具备优势,且钢管板桩结构可更好的适应码头的大型化和深水化发展,在类似工程设计中可优先采用钢管板桩结构。  相似文献