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marine invasion
相关语句
  海侵
     Holocene Marine Invasion Event and Climate Change in North Jiangsu
     江苏北部全新世海侵事件和气候变化
短句来源
     In the region of Laizhou gulf where disaster of marine invasion is very serious, distribution and migration of salinity and Na~+,Cl~-,Ca~(2+),Mg~(2+),K~+ in 0~40 cm soil irrigated by seawater were investigated, to attain the most fitting irrigation requirement.
     对在海侵灾害最严重的莱州湾地区,在油葵生育期内利用不同浓度的海水直接灌溉两次,研究0~40cm土层土壤盐分及Na+、Cl-、Ca2+、Mg2+、K+含量的分布、迁移规律,为确定合适的灌溉定额和灌溉次数提供最基础的技术参数。
短句来源
     To the period of 2200aBP~1000aBP,the second Holocene marine invasion happened in the region of Jianhu,whose scale was smaller than the first one.
     至 2 2 0 0aBP~ 10 0 0aBP期间 ,建湖地区又发生全新世第二次海侵 ,但其规律远小于第一次。
短句来源
     The red layers in member Es 3 3(shallow water remarks)and the depositional sequence of evaporating rocks in this depression show that the salt and gypsum in this depression were formed from the evaporating marine invasion shallow water.
     沙三3亚段出现的红色地层 (浅水标志 )和该凹陷的蒸发岩的沉积序列特征表明 ,东濮凹陷的盐岩为海侵的浅水蒸发盐。
短句来源
     When the subsiding of the basin base became slow down,no marine invasion was found and the basin was dominated by a peat swamp environment in which coal beds were deposited.
     盆地基底沉降速率较慢、无海侵作用时,盆地为泥炭沼泽环境,主要发育煤层。
短句来源
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  海水入侵
     In Late Pleistocne Epoch, Taihu Lake Plain suffered marine invasion three times, making fluviolacustrine sedimentary environment become tidal flat sedimentary environment three times.
     晚更新世时期 ,太湖平原三次遭受海水入侵 ,以致河湖沉积环境曾三度变为潮坪沉积环境。
短句来源
  “marine invasion”译为未确定词的双语例句
     GENESIS AND CONTROLLING MEASURES OF MARINE INVASION IN LIAONING PROVINCE
     辽宁省海水入侵成因及防治措施
短句来源
     Ballast water discharges lead to marine invasion between geographically isolated water, and are the main approach to spreading harmful microorganism.
     船舶压载水的给排过程是造成地理性隔离水体间海洋生物传播的最主要途径。
短句来源
     Ballast water discharges lead to marine invasion between geographically isolated water, and are the main approach to spreading harmful microorganism.
     船舶压载水是外来生物入侵最主要传播途径。
短句来源
     Ballast water discharges lead to marine invasion between geographically isolated water,and are the main approach to spreading harmful microorganism.
     船舶压载水排放造成了地理性隔离水体间的生物入侵 ,是有害微生物传播的最主要途径。
短句来源
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  marine invasion
The Roles of Competition and Disturbance in a Marine Invasion
      
The role of parasites in a marine invasion was assessed by first examining regional patterns of trematode parasitism in the introduced Japanese mud snail, Batillaria cumingi (= B.
      
We identify the Northeast Pacific Ocean (NEP; northern California to British Columbia) as a model system for analyzing patterns of marine invasion success in cool temperate waters.
      
Blitzkrieg in a Marine Invasion: Caulerpa racemosa var.
      
Where data exist, I evaluate these examples in terms of lessons marine invasion biologists can glean from the rich history of terrestrial biocontrol, and explicitly contrast agroecosystems with invaded marine habitats.
      
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Abstract The geochemical character of every kind of rocks(ores):Sr/Ba, Mn/Fe, Co/Ni,As,Ce/Ce,Eu/Eu,anomalous Ce,δi3C and δ18O in P- bearing rock sereis in Xingshen phosphate deposit show that:In the early sedimentary stage of the p-bearing rock series,manganiferous dolomite was formed by the effection of glacier fresh water;in the middle sedimentary stage,since the developing of marine invasion and the deepening of water body,phosphorite had been accumulated due to bred a great deal of organism in the...

Abstract The geochemical character of every kind of rocks(ores):Sr/Ba, Mn/Fe, Co/Ni,As,Ce/Ce,Eu/Eu,anomalous Ce,δi3C and δ18O in P- bearing rock sereis in Xingshen phosphate deposit show that:In the early sedimentary stage of the p-bearing rock series,manganiferous dolomite was formed by the effection of glacier fresh water;in the middle sedimentary stage,since the developing of marine invasion and the deepening of water body,phosphorite had been accumulated due to bred a great deal of organism in the semi-enclosed low reduction-blightly oxidation enviroment; in the late sedimentary stage,migmatized dolomite was formed result from the air fresh water effection and the marine regression,and then,the p-forming history ended.

兴神磷矿含磷岩系各类岩(矿)石Sr/Ba,Mn/Fe,Co/Ni,As,Ce/Ce“,Eu/Ell刮,异常Ce,6“C,61‘O等地球化学特点表明,含磷岩系沉积早期受冰)I淡水影响形成合锰白云岩;中期海馒规模扩大,水体加深,在半封闭的低能还原一弱氧化环境中.生物大量繁殖形成磷块岩堆积;晚期出现海退,在大气淡水影响下形成混合岩化白云岩结束整个成磷历史。

Sinian system and Lower Cambrian series in Jinzhou area,Daian,can be divied intoSinian Liaonan ultra-sequence and Early Cambrian Manjiatan ultra-sequence,and can be sub-divided into Nanguanling ,Qipanmo, Luhai,Getun,Dalinzi and Caotuozi sequences.The rela-tionship between every two sequences were unconformable, which the types included subaeri-al exposure belt,coastal exposure belt and marine invasion plane. Each sequence was consist-ed of marine invasion and high water level system domains,which...

Sinian system and Lower Cambrian series in Jinzhou area,Daian,can be divied intoSinian Liaonan ultra-sequence and Early Cambrian Manjiatan ultra-sequence,and can be sub-divided into Nanguanling ,Qipanmo, Luhai,Getun,Dalinzi and Caotuozi sequences.The rela-tionship between every two sequences were unconformable, which the types included subaeri-al exposure belt,coastal exposure belt and marine invasion plane. Each sequence was consist-ed of marine invasion and high water level system domains,which the former was ret-rograding strata, the latter was prograding strata, but starvated member between them wasmainly accretion strata,all the changing was related with relative sea level and global sea lev-el,On the base of above features,the paper set up a regional stratigraphic framework and in-dicated the sedimentary scope then mainly was within the plateform which partly developeddeep-water continental shelf basins.

大连金州地区震旦纪、早寒武世地层发育。本区该套地层可划分为震旦纪辽南超层序和早寒武世满家滩超层序,在其内部又可进一步划分为南关岭层序、棋盘磨层序、陆海层序、葛屯层序、大林子层序和草坨子层序六个层序地层单位。各层序之间均为不整合,其类型包括陆上暴露带、海岸暴露带及海侵面。每个层序仅由海侵体系域和高水位体系域组成。前者为退积地层结构,后者为进积地层,而中间饥饿段却表现为以加积为主,所有变化都与相对海平面及全球海平面变化有关。在此基础上,建立了区域地层格架,指出了本区该时期沉积范围主要在台地之内部(中陆架),局部发育深水陆棚盆地。

Reaction path simulation technique that started its development within recent20 years is an important method in quantitatively studying the geochemical evolution ofgroundwater. This paper discusses the difference of reaction path simulation and mass balance simulation. The authors put forward to adopt step simulation for complicated waterflow system and dissolution of soil salt synthetic system for evaporation concentration andinfluence of marine invasion which may be master process of shallow salt water...

Reaction path simulation technique that started its development within recent20 years is an important method in quantitatively studying the geochemical evolution ofgroundwater. This paper discusses the difference of reaction path simulation and mass balance simulation. The authors put forward to adopt step simulation for complicated waterflow system and dissolution of soil salt synthetic system for evaporation concentration andinfluence of marine invasion which may be master process of shallow salt water forming.The process of geochemical evolution of shallow groundwater in the studied area was expound.

反应路径模拟技术是近十几年发展起来的定量研究地下水地球化学演化的重要方法。文中讨论了反应路径模拟与质量平衡模拟的差异,提出了对复杂水流系统采取分段模拟,以及对浅层成水形成的主要作用即蒸发浓缩作用和海侵的影响采用土壤盐类综合体的溶解来表征的处理方法,论述了研究区浅层地下水的地球化学演化过程。

 
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