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文学语言是一种多重符号,它“一语双关”。文学语言所表达的意义可以分为表层意义和深层意义。表层意义构成形象和图画,深层意义构成情感、思维或哲理。在文学作品中用来表现深层意义的艺术手法主要有:“不着一字”法、双关法、象征法、析字法。表层意义是固定的、不变的;而深层意义则是流动的、变化的。读者在欣赏文学作品时,应透过字里行间去领略作者的言外之意,去理解作品所蕴合的深层意义。 相似文献
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厦门—金门海域表层沉积物中HCHs,DDTs和PCBs的含量与分布 总被引:6,自引:0,他引:6
1995年10月对厦门-金门海域表层沉积物中的有机氯农药(HCHs和DDTs)及多氯联苯(PCBs)的含量与分布进行调查研究,HCHs,DDTs和PCBs的含量范围分别为0.03~0.48mg/g,2.97~9.16ng/g和0.02~0.11ng/g对其分布形式,残留水平以及组成等进行了评价与探讨,结果表明,厦门-金门海域基本上未受到HCHs和PCBs的污染,只受到DDT的轻度污染,但是,DDT 相似文献
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运用化学分析和藻类生物测定相结合的方法,对样口藻类可利用颗粒磷(AAPP)进行定量估算,结果表明,取得了厦门湾,泉州湾和黄河口样品中AAPP为61~142mg/kg占样品总磷之8.0%~20.2%,样品中非磷灰石无机磷是潜在生物可利用磷,磷灰石无机磷则难以被藻类利用,AAPP高低主要与样品物源区气候环境条件下,磷的矿物组成,化学存在形态等有关,而与实验藻种无关,推荐用0.1mol/LNaOH~1. 相似文献
6.
天津塘沽驴驹河海岸带海水和沉积物现状调查 总被引:3,自引:0,他引:3
通过对天津塘沽区驴驹河海岸带5个海水样品和16个沉积物样品的采样分析,对该区的海水和沉积物环境质量状况进行了评价。结果表明,该水域主要受到了油类和重金属汞(Hg)的污染,其中油类和汞的污染指数平均值分别为2.698和6.64;砷(As)和石油烃是沉积物的主要污染物,砷的污染指数平均值为0.904,石油烃的污染指数平均值为1.111。研究成果为该区进一步的生态修复提供了科学依据。 相似文献
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林婉珍 《福建师范大学学报(自然科学版)》2005,21(3):39-42
采用化学连续提取法对福州西湖两个柱状沉积物样品中垂向不同形态磷进行分级提取分析.结果表明:1#样品表层沉积物总磷含量在830μg/g左右,垂向各层总磷呈“S”状分布;2#样品表层沉积物总磷含量在700μg/g左右,垂向各层总磷呈“7”状分布.两个柱状沉积物垂向各层均以无机磷为主,占总磷含量的80%~90%,其中铁磷含量远远高于铝磷和钙磷的含量,占总磷量的50%~60%.两个柱状沉积物垂向各层中闭蓄态磷含量很低,说明沉积物中自然来源的磷很少,主要以人为输入为主,垂向各层磷形态和含量的不同,反映了不同时期和不同程度的人为输入磷的污染. 相似文献
8.
Quaternary high-resolution opal record and its paleoproductivity implication at ODP Site 1143,southern South China Sea 总被引:4,自引:0,他引:4
WANGRujian LIJian 《科学通报(英文版)》2003,48(4):363-367
The correlation of opal content and MAR with oxygen isotopic records of benthonic foraminifera at Site 1143, southern South China Sea indicates that,since about 900 ka,the increasing opal content and MAR during the interglacial periods is inferred to reflect the bigher surface productivity ,for the intensified summer monsoon during the interglacial periods would result in the enhanced upwelling and nutrient supply,Time-sequence spectral analyses of oxygen isotopic record ,opal content and MAR at intervals of 0-900 ka reveal that the changes of surface productivity were dominantly forced by the variations of the earth orbital cycles. 相似文献
9.
LU Anhuai GAO Xiang QIN Shan & WANG ChangqiuDepartment of Geology Peking University Beijing . China Correspondence should be addressed to Lu Anhuai 《科学通报(英文版)》2003,48(9):920-923
The Xiangtan manganese deposit (XTM) used to be considered a supergene oxide manganese ore in South China. We reported a new identification of the naturally outcropping cryptomelane by examining the physical, chemical and structural features of the XTM supergene oxide manganese ore. The MnO2 content was over 90%, K2O more than 3%, and water from 2.2%-3.1% which is similar to one in zeolite. The cell parameters of the cryptomelane were given as a0 = 0.9974 nm, b0 = 0.2863 nm, c0 = 0.9693 nm and β= 91.47°. There was a larger pseduotetragonal tunnel in the natural cryptomelane that was formed by [MnO6] octahedral double chains with aperture of 0.462×0.466 nm2, filled with K cations resulting in some Mn3+ substituting for Mn4+ to balance the negative charges of structure. The finding is important not only for prospecting manganese resources in South China, but also in application of octahedral molecular sieve of natural cryptomelane as that developed in the tetragonal molecular sieve of natural zeolite o 相似文献
10.
YANGBao A.Braeuning SHIYafeng ZHANGJiawu 《科学通报(英文版)》2003,48(14):1446-1450
The paleoclimate data recovered from ice cores,tree rings and lake sediments indicate regional features of cfimatic change on the Tibeta n Plateau (TP) during the last 2000 years. The composite temperature reconstructions in-dicate that several main climatic episodes, such as the “LittleIce Age“ between 1400 and 1900, the “Medieval Warm Pe-riod“ in 1150-1400, a less warm period in 800-1100, and an earlier cold period between the 3rd and 5th centuries,occurred in the TP. In addition, temperature varied from region to region. The period from AD 800 to 1100, which waswarm in northeastern TP, was contemporaneous with cool-ing in the western and southern TP. The southern TP ex-perienced warming between 1150 and 1400. For western TP,the δ^18O records of the Guliya ice core indicate that the pe-Hod 1250-1500 witnessed a clear warming. Large-scaletrends in the temperature history from northeastern TP aremore similar to those in eastern China than are the trendsfrom the Guliya ice cap far to the west and southern TP. The most prominent similarities between the temperature varia-tions of the TP and eastern China are such cold phases as 1100-1150, 1500-1550, 1650-1700 and 1800-1850, andthe latter three cold events match with three widespreadg lacial advances which occurred on the TP during the Little Ice A2e. 相似文献