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標(biāo)題: Titlebook: Atmospheric Methane: Sources, Sinks, and Role in Global Change; M. A. K. Khalil (Professor and Director) Conference proceedings 1993 Sprin [打印本頁]

作者: malfeasance    時(shí)間: 2025-3-21 16:28
書目名稱Atmospheric Methane: Sources, Sinks, and Role in Global Change影響因子(影響力)




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作者: 尋找    時(shí)間: 2025-3-21 22:49

作者: 盲信者    時(shí)間: 2025-3-22 00:36

作者: Confidential    時(shí)間: 2025-3-22 04:36
Atmospheric Methane Concentrationsties at Cape Meares, Oregon (Rasmussen and Khalil, 1981). Since that time, more detailed and extensive data sets have allowed estimation of sources and sinks of methane on the global scale. As attempts are made to refine these estimates, the value of the current databases will be greatly increased,
作者: entitle    時(shí)間: 2025-3-22 09:20
Biological Formation and Consumption of Methanemarine and freshwater sediments, and the gastrointestinal tract of animals (Whitman et al., 1992). This chapter describes the conditions that lead to biogenic methane formation in natural environments, the metabolic pathways and interactions that lead to methanogenesis, and the implications of these
作者: 興奮過度    時(shí)間: 2025-3-22 15:39
Stable Isotopes and Global Budgetssion the yearly 1% rise in lower tropospheric methane mixing ratios (e.g., Blake and Rowland, 1988), and we have adequate, basic global coverage of atmospheric methane latitudinal variation. Mesoscopically, we are able to roughly estimate the various source strengths, e.g., from wetlands, agricultur
作者: MAZE    時(shí)間: 2025-3-22 17:08
Methane Sinks Distributionear. Most of the methane is removed by reacting with tropospheric OH radicals; lesser amounts are removed by soils and stratospheric oxidation by OH, O(.D), and minor reactions. This chapter is on the removal rate of CH. and its variability in space and time.
作者: 虛弱    時(shí)間: 2025-3-23 01:15
Sources of Methane: An Overviewe who want to reduce methane in the atmosphere or prevent it from increasing, controlling the sources is perhaps the only practical approach. Accordingly,.a significant portion of this book is devoted to estimating the global and regional emission rates. The purpose of this chapter is to introduce t
作者: prosperity    時(shí)間: 2025-3-23 04:26
Ruminants and Other Animalsnt animal contribution to atmospheric methane has been recognized for some time. Approximately 95 percent of animal methane emissions are accounted for by ruminants. The emphasis in this paper will therefore be primarily focused on these animals.
作者: 催眠藥    時(shí)間: 2025-3-23 07:19

作者: stratum-corneum    時(shí)間: 2025-3-23 10:15

作者: incision    時(shí)間: 2025-3-23 16:01
Biomass Burning 1991a). The burning of living and dead biomass is a very significant global source of atmospheric gases and particulates. Crutzen and colleagues were the first to assess biomass burning as a source of gases and particulates to the atmosphere (Crutzen et al., 1979; and Seiler and Crutzen, 1980). How
作者: 負(fù)擔(dān)    時(shí)間: 2025-3-23 21:40
Wetlands, 1991), accounting for ~20% of the current global annual emission of ~450–550 Tg (10. g). Measurements of methane from Greenland and Antarctic ice cores indicate atmospheric concentrations of ~350 ppbv during the Last Glacial Maximum rising to 650 ppbv during the pre-industrial Holocene (Stauffer e
作者: Leisureliness    時(shí)間: 2025-3-24 01:08

作者: 狼群    時(shí)間: 2025-3-24 04:11

作者: Venules    時(shí)間: 2025-3-24 08:53
Sources and Sinks of Methaneasmussen, 1990). The current annual rate of increase of about 0.8% year. is attributed to increases in industrial and agricultural emissions since some key natural sources (e.g., wetlands and marshes) have been reduced due to development pressure, decreasing their area in various parts of the world
作者: Urgency    時(shí)間: 2025-3-24 11:29

作者: BET    時(shí)間: 2025-3-24 16:08

作者: encyclopedia    時(shí)間: 2025-3-24 22:21

作者: 光亮    時(shí)間: 2025-3-25 00:29

作者: 爭論    時(shí)間: 2025-3-25 05:31
Vincenzo Catrambone,Gaetano Valenzant animal contribution to atmospheric methane has been recognized for some time. Approximately 95 percent of animal methane emissions are accounted for by ruminants. The emphasis in this paper will therefore be primarily focused on these animals.
作者: 袖章    時(shí)間: 2025-3-25 07:35
Funktionen Mehrerer Ver?nderlicher, 1991), accounting for ~20% of the current global annual emission of ~450–550 Tg (10. g). Measurements of methane from Greenland and Antarctic ice cores indicate atmospheric concentrations of ~350 ppbv during the Last Glacial Maximum rising to 650 ppbv during the pre-industrial Holocene (Stauffer et al., 1988; Chappellaz et al., 1990).
作者: Inelasticity    時(shí)間: 2025-3-25 15:39

作者: 古老    時(shí)間: 2025-3-25 17:57

作者: moratorium    時(shí)間: 2025-3-25 23:27
Hans Martin Reimann,Thomas RychenerThis chapter identifies and describes major industrial sources of methane (CH.) emissions. For each source type examined, CH. release points are identified and a detailed discussion of the factors affecting emissions is provided. A summary and discussion of available global and country-specific CH. emissions estimates are also presented.
作者: Yag-Capsulotomy    時(shí)間: 2025-3-26 03:46
An Introduction to Atmospheric MethaneI have two purposes in writing this chapter. The first is to give a brief eyewitness report on the evolution of the current knowledge of methane trends, and the second is to provide a guide to the logic behind this book.
作者: 召集    時(shí)間: 2025-3-26 05:24

作者: 古老    時(shí)間: 2025-3-26 10:58

作者: 拋棄的貨物    時(shí)間: 2025-3-26 13:44
Nato ASI Subseries I:http://image.papertrans.cn/b/image/164628.jpg
作者: Bmd955    時(shí)間: 2025-3-26 19:23
https://doi.org/10.1007/978-3-642-84605-2Air Pollution; Atmospheric Methane; Global Warming; Globale Erw?rmung; Greenhouse gas; Luftverschmutzung;
作者: 獨(dú)行者    時(shí)間: 2025-3-26 22:54

作者: Negligible    時(shí)間: 2025-3-27 02:02
Fitnessball, Gymnastiball und Pezziballeographical distribution of natural and human sources, biogeochemical and ecosystem dynamics, human agricultural and industrial practices, and atmospheric chemistry and dynamics. For an understanding of the global methane cycle, it is necessary to develop and apply methods that are suitable for meas
作者: 聽寫    時(shí)間: 2025-3-27 07:56
Fitnessball, Gymnastiball und Pezziballatic survey only since 1979. The data from this time up to 1983 indicate an increasing trend at a rate of about 1% per year (Rasmussen and Khalil, 1986; Steele et al., 1987; Blake and Rowland, 1988). The most recent measurements indicate a slowing of the global accumulation of atmospheric CH. (Khali
作者: GRAVE    時(shí)間: 2025-3-27 12:30

作者: 吸氣    時(shí)間: 2025-3-27 15:13
https://doi.org/10.1007/978-3-662-43659-2ties at Cape Meares, Oregon (Rasmussen and Khalil, 1981). Since that time, more detailed and extensive data sets have allowed estimation of sources and sinks of methane on the global scale. As attempts are made to refine these estimates, the value of the current databases will be greatly increased,
作者: relieve    時(shí)間: 2025-3-27 17:52

作者: 一回合    時(shí)間: 2025-3-27 22:39

作者: gregarious    時(shí)間: 2025-3-28 05:35
Vincenzo Catrambone,Gaetano Valenzaear. Most of the methane is removed by reacting with tropospheric OH radicals; lesser amounts are removed by soils and stratospheric oxidation by OH, O(.D), and minor reactions. This chapter is on the removal rate of CH. and its variability in space and time.
作者: Narcissist    時(shí)間: 2025-3-28 08:22

作者: 生氣地    時(shí)間: 2025-3-28 13:31
Vincenzo Catrambone,Gaetano Valenzant animal contribution to atmospheric methane has been recognized for some time. Approximately 95 percent of animal methane emissions are accounted for by ruminants. The emphasis in this paper will therefore be primarily focused on these animals.
作者: altruism    時(shí)間: 2025-3-28 16:12

作者: oblique    時(shí)間: 2025-3-28 18:47

作者: 不合    時(shí)間: 2025-3-29 01:56

作者: arbovirus    時(shí)間: 2025-3-29 04:49

作者: Contracture    時(shí)間: 2025-3-29 08:12
Hans Martin Reimann,Thomas Rychenerm these sources suggest approximately 70 (54–95) Tg/yr globally or 14% of total global CH. emissions of 500 Tg/yr (IPCC, 1992). This chapter begins with a brief overview of how CH. is generated from the anaerobic decomposition of waste and then discusses generation of CH. in detail in landfills, was
作者: 經(jīng)典    時(shí)間: 2025-3-29 13:23

作者: Adjourn    時(shí)間: 2025-3-29 15:43

作者: MAOIS    時(shí)間: 2025-3-29 21:39
Atmospheric Methane Concentrationsties at Cape Meares, Oregon (Rasmussen and Khalil, 1981). Since that time, more detailed and extensive data sets have allowed estimation of sources and sinks of methane on the global scale. As attempts are made to refine these estimates, the value of the current databases will be greatly increased, as will the need for more current data.
作者: 脫離    時(shí)間: 2025-3-30 00:31

作者: homocysteine    時(shí)間: 2025-3-30 04:11

作者: Exposure    時(shí)間: 2025-3-30 12:05

作者: Criteria    時(shí)間: 2025-3-30 16:00

作者: Glycogen    時(shí)間: 2025-3-30 17:56
Isotopic Abundances in the Atmosphere and Sourcesme as now. The lifetime was mostly determined by the fluxes based on the emissions inventories. This approach does not use the lifetime as a constraint nor contribute to the knowledge of the major sources, which have significant uncertainties in the estimates based on emissions inventories. A better
作者: palpitate    時(shí)間: 2025-3-30 22:44
Rice Agriculture: Factors Controlling Emissionshich is of biogenic origin (Bouwman, 1990). Methane emissions from wetland rice agriculture have been estimated up to 170 Tg/yr, which account for approximately 26% of the global anthropogenic methane budget. Flooded ricefields are probably the largest agricultural source of methane, followed by rum
作者: 冥想后    時(shí)間: 2025-3-31 02:05

作者: TRUST    時(shí)間: 2025-3-31 07:59

作者: 顯而易見    時(shí)間: 2025-3-31 09:34
Slide-Training mit der Rutschmatte: FLOWIN?me as now. The lifetime was mostly determined by the fluxes based on the emissions inventories. This approach does not use the lifetime as a constraint nor contribute to the knowledge of the major sources, which have significant uncertainties in the estimates based on emissions inventories. A better
作者: 含鐵    時(shí)間: 2025-3-31 13:26

作者: 出處    時(shí)間: 2025-3-31 20:20
Fitnessball, Gymnastiball und Pezziballnsland et al., 1985; Zander et al., 1989) provides additional data of global concentrations for a few specific years (1951, 1975, 1981,. 1984–87) and shows a mean increase of about 30% over the past 40 years. This long-term accumulation of CH. in the atmosphere is related to human activities, particularly from agricultural activities.
作者: Culpable    時(shí)間: 2025-3-31 22:41
Vincenzo Catrambone,Gaetano Valenzahere-atmosphere interface. This knowledge deficit includes our understanding of both release and uptake process-groups. Control of methane emissions to the atmosphere requires that we reliably characterize these source-sink relationships.
作者: 托人看管    時(shí)間: 2025-4-1 05:04

作者: 合法    時(shí)間: 2025-4-1 07:59

作者: 內(nèi)部    時(shí)間: 2025-4-1 10:41

作者: mutineer    時(shí)間: 2025-4-1 16:52
Minor Sources of Methaned, and some may have been overlooked hitherto. More detailed discussions of these sources are provided by Hovland et al. (1993), Lacroix (1993), Lambert and Schmidt (1993), Rouland et al. (1993), Smith et al. (1993), and Khalil et al. (1993).




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