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標(biāo)題: Titlebook: Geochemistry of Organic Matter in the Ocean; Evgenii A. Romankevich Book 1984 Springer-Verlag Berlin Heidelberg 1984 Matter.Ocean.chemistr [打印本頁(yè)]

作者: Constrict    時(shí)間: 2025-3-21 16:40
書目名稱Geochemistry of Organic Matter in the Ocean影響因子(影響力)




書目名稱Geochemistry of Organic Matter in the Ocean影響因子(影響力)學(xué)科排名




書目名稱Geochemistry of Organic Matter in the Ocean網(wǎng)絡(luò)公開度




書目名稱Geochemistry of Organic Matter in the Ocean網(wǎng)絡(luò)公開度學(xué)科排名




書目名稱Geochemistry of Organic Matter in the Ocean被引頻次




書目名稱Geochemistry of Organic Matter in the Ocean被引頻次學(xué)科排名




書目名稱Geochemistry of Organic Matter in the Ocean年度引用




書目名稱Geochemistry of Organic Matter in the Ocean年度引用學(xué)科排名




書目名稱Geochemistry of Organic Matter in the Ocean讀者反饋




書目名稱Geochemistry of Organic Matter in the Ocean讀者反饋學(xué)科排名





作者: ACME    時(shí)間: 2025-3-21 22:59
978-3-642-49966-1Springer-Verlag Berlin Heidelberg 1984
作者: CLIFF    時(shí)間: 2025-3-22 01:22
International Human Resource Management,tate in the ocean waters, and in the sediments. Inorganic and organic forms of these elements are the most essential biogenic constituents of ocean waters, and being functionally involved in the processes of living organisms, are subjected to a rapid turnover.
作者: congenial    時(shí)間: 2025-3-22 08:37
Nitrogen and Phosphorus in the Process of Sedimentogenesis,tate in the ocean waters, and in the sediments. Inorganic and organic forms of these elements are the most essential biogenic constituents of ocean waters, and being functionally involved in the processes of living organisms, are subjected to a rapid turnover.
作者: 思想靈活    時(shí)間: 2025-3-22 10:51

作者: Incisor    時(shí)間: 2025-3-22 16:36

作者: Incisor    時(shí)間: 2025-3-22 19:06
Carbon of Dissolved Organic Matter in the Ocean,ve analysis, OM is classified at present in the majority of works only as dissolved and particulate (suspended). Definition of the term “dissolved organic matter” (DOM) means distinguishing between these two arbitrarily identified forms of organic compounds in natural waters. No uniform opinion prev
作者: 鉤針織物    時(shí)間: 2025-3-22 23:51
Carbon of Particulate Organic Matter,in the filters with 0.45 – 1 μm pore size or in separators. Large OM particles in natural waters are present in an extremely scattered state and are usually not to be found in filtration particulate suspensates. Their quantity in the ocean, compared to the bulk of OM is insignificant, but they play
作者: 出價(jià)    時(shí)間: 2025-3-23 03:59

作者: heterodox    時(shí)間: 2025-3-23 08:45

作者: 不可救藥    時(shí)間: 2025-3-23 10:15

作者: 追逐    時(shí)間: 2025-3-23 17:17

作者: Heart-Rate    時(shí)間: 2025-3-23 20:50
Chemical Transformations of Lipids During Sedimentogenesis, lipids is the presence of higher alkyl radicals in the molecules. The sources of lipids in the seas and oceans are the auto- and heterotrophic organisms inhabiting the marine environment. The community of living organisms produces annually in the world oceans 7 × 10. tons of fatty substances (Bogor
作者: ADORN    時(shí)間: 2025-3-23 22:55

作者: 反省    時(shí)間: 2025-3-24 06:00

作者: Iatrogenic    時(shí)間: 2025-3-24 09:42
Duncan Waite,Lejf Moos,Chulsub Lewe to put to rational use its nutritive, mineral and power resources. The avalanche-like growth of information about various processes in the ocean was the result of new opportunities for its study, using up-to-date research ships, earth satellites and submersible vessels, and of the progress achieve
作者: 創(chuàng)作    時(shí)間: 2025-3-24 13:36

作者: MANIA    時(shí)間: 2025-3-24 15:54
https://doi.org/10.1007/978-1-349-24069-2ve analysis, OM is classified at present in the majority of works only as dissolved and particulate (suspended). Definition of the term “dissolved organic matter” (DOM) means distinguishing between these two arbitrarily identified forms of organic compounds in natural waters. No uniform opinion prev
作者: 憤憤不平    時(shí)間: 2025-3-24 19:50

作者: 極小量    時(shí)間: 2025-3-25 00:24
https://doi.org/10.1007/978-3-030-82315-3ended matter that sinks to the bottom, which in terms of C. approximates (1.2 – 3.7) × 10. tons yearly. The decomposition of the aquatic organic precipitation is practically the sole energy source of biogeochemical processes of authigenous mineral formation, that results in element dissemination and
作者: addict    時(shí)間: 2025-3-25 07:00

作者: 譏諷    時(shí)間: 2025-3-25 10:52

作者: 媽媽不開心    時(shí)間: 2025-3-25 15:31
https://doi.org/10.1007/978-3-540-70527-7nd are the major source of energy for living organisms, accounting for over 60% of their energy requirements. Carbohydrates exist in living organisms in combined forms, being associated with proteins, lipids and nucleic acids, and constitute intricate high molecular complexes which form the basis of
作者: Generator    時(shí)間: 2025-3-25 18:54

作者: vitreous-humor    時(shí)間: 2025-3-25 21:15

作者: BROTH    時(shí)間: 2025-3-26 01:20

作者: 薄膜    時(shí)間: 2025-3-26 06:24

作者: acrophobia    時(shí)間: 2025-3-26 10:33

作者: Acupressure    時(shí)間: 2025-3-26 13:35

作者: Consensus    時(shí)間: 2025-3-26 17:26
https://doi.org/10.1007/978-3-031-15866-7e extracted from the sediments unless the mineral matrix is destroyed. The living, normally functioning organisms do not contain FA and HA. Such substances may be formed in some quantity as the metabolic products of exchange in the organisms or they may be the result of the alkaline hydrolysis of na
作者: thrombosis    時(shí)間: 2025-3-26 22:09

作者: 施加    時(shí)間: 2025-3-27 03:36

作者: calamity    時(shí)間: 2025-3-27 09:22

作者: thrombus    時(shí)間: 2025-3-27 10:01

作者: 多山    時(shí)間: 2025-3-27 15:33
Conclusion,n of OM on the molecular and atomic level; fourthly, a significant improvement of sampling methods and techniques and, finally, the supplementation of the formerly dominant chemico-analytical methods with the new and/or improved biogeochemical ones.
作者: habile    時(shí)間: 2025-3-27 18:00
The European System of Human Rightsov 1971). A certain portion of these lipids reaches the aquatic environment with allochthonous OM; this comprises natural lipid compounds and the constituents of oil (Goldberg 1975, Cowell 1976, Nesterova and Simonov 1979, Nemirovskaya and Nesterova 1982).
作者: Traumatic-Grief    時(shí)間: 2025-3-28 01:29

作者: Lumbar-Stenosis    時(shí)間: 2025-3-28 05:07
tion of various forms of organic matter in the ocean: dissolved, colloidal, organic matter sus- pended in particles and that contained in bottom sediments and in interstitial waters. The appropriate evidence is found in hundreds of articles and several re- view works, such as Andersen (1977), Biogeo
作者: RUPT    時(shí)間: 2025-3-28 08:29
Duncan Waite,Lejf Moos,Chulsub Lew the result of new opportunities for its study, using up-to-date research ships, earth satellites and submersible vessels, and of the progress achieved in research techniques and in quantitative methods of studying the oceanosphere and the hydrosphere as a whole.
作者: conduct    時(shí)間: 2025-3-28 13:36

作者: 堅(jiān)毅    時(shí)間: 2025-3-28 16:18
https://doi.org/10.1007/978-3-540-70527-7in combined forms, being associated with proteins, lipids and nucleic acids, and constitute intricate high molecular complexes which form the basis of living matter. They are incorporated in the cells in forms of various derivatives, and are functionally involved in the structure, energy- and growth-regulating processes of all living organisms.
作者: Albumin    時(shí)間: 2025-3-28 20:47

作者: Osteons    時(shí)間: 2025-3-29 01:21

作者: galley    時(shí)間: 2025-3-29 04:35
Carbohydrates,in combined forms, being associated with proteins, lipids and nucleic acids, and constitute intricate high molecular complexes which form the basis of living matter. They are incorporated in the cells in forms of various derivatives, and are functionally involved in the structure, energy- and growth-regulating processes of all living organisms.
作者: 大雨    時(shí)間: 2025-3-29 07:25

作者: 喪失    時(shí)間: 2025-3-29 13:55

作者: 藝術(shù)    時(shí)間: 2025-3-29 15:37
The Effects of IHRM on Employee Outcomes,— 46 – 88% (averaging 72%), zoobenthos — 72 – 84%, bacteria — about 75%, phytobenthos — 7 – 36% (averaging 17%). Proteins constitute only 70 – 85% of the nitrogenous substances in marine organisms. These seem to be overestimates, although on the whole they correctly depict the total content of amino acids in marine organisms (Fig. 48).




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