marine sediment

基本解釋

Microscopic organisms settle to the seafloor and accumulate in marine mud, thus marine sediment was formed.
微生物生存于海底，并聚積在海底的淤泥之中，這樣便形成了海洋沉積物。
Significant progress in the establishment of a unified marine sediment dynamics has been made through the joint effort by physical oceanographers, coastal engineers and marine geologists.
海洋沉積動力學(xué)正在打破傳統(tǒng)，走向海洋工程學(xué)、物理海洋學(xué)和地質(zhì)學(xué)的聯(lián)合，共同建立一門綜合性的、統(tǒng)一的沉積動力學(xué)。
Besides temperature and pressure, the controlling factors for gas hydrate stability also include pore water composition, gas concentration in the fluid and marine sediment types in the seafloor.
海洋天然氣水合物的生成除了受溫度和壓力的影響外，還要受到孔隙水的化學(xué)組成、流體中氣體的濃度及沉積物類型的影響。

海洋沉積物
Microbial diversity in marine sediment is an important component of marine biodiversity,it plays an important role in geochemical cycle.
海洋沉積物微生物多樣性是海洋生物多樣性的重要組成部分,在海洋生物地球化學(xué)循環(huán)中發(fā)揮著重要作用。
地球科學(xué)
海洋沉積物
Actual marine sediment cores will be used in similar experiments to study the relationship between gas hydrate saturation and acoustic parameters. Parameters of the models determined by experiments will be useful in practical application.
在掌握實(shí)驗(yàn)技術(shù)的基礎(chǔ)上,使用實(shí)際的海洋沉積物巖心進(jìn)行同樣的實(shí)驗(yàn),研究水合物飽和度與聲學(xué)參數(shù)的響應(yīng)關(guān)系,確定各理論方程中參數(shù)的取值,將得到實(shí)際的應(yīng)用。
海底沉積物
Factors that can influent the distribution and transportation of suspended matter in the surface layer are composed of topography, marine sediment properties, runoffs, thermocline, wind, waves, circulations and so on.
影響表層懸浮體分布和輸運(yùn)的因素包括地形、海底沉積物類型、徑流、躍層、風(fēng)浪以及環(huán)流等等,海水中的懸浮體在這些因素的綜合作用下呈現(xiàn)出上述的空間分布特征和季節(jié)變化規(guī)律。
海洋底泥
海相沉積
海洋沉積
海洋沈積物
海相沉積物