標題: Titlebook: Carbon and Nitrogen in the Terrestrial Environment; R. Nieder,D. K. Benbi Book 2008 Springer Science+Business Media B.V. 2008 Greenhouse g [打印本頁] 作者: GLAZE 時間: 2025-3-21 18:00
書目名稱Carbon and Nitrogen in the Terrestrial Environment影響因子(影響力)
書目名稱Carbon and Nitrogen in the Terrestrial Environment影響因子(影響力)學(xué)科排名
書目名稱Carbon and Nitrogen in the Terrestrial Environment網(wǎng)絡(luò)公開度
書目名稱Carbon and Nitrogen in the Terrestrial Environment網(wǎng)絡(luò)公開度學(xué)科排名
書目名稱Carbon and Nitrogen in the Terrestrial Environment被引頻次
書目名稱Carbon and Nitrogen in the Terrestrial Environment被引頻次學(xué)科排名
書目名稱Carbon and Nitrogen in the Terrestrial Environment年度引用
書目名稱Carbon and Nitrogen in the Terrestrial Environment年度引用學(xué)科排名
書目名稱Carbon and Nitrogen in the Terrestrial Environment讀者反饋
書目名稱Carbon and Nitrogen in the Terrestrial Environment讀者反饋學(xué)科排名
作者: Mendacious 時間: 2025-3-21 21:03 作者: 冥想后 時間: 2025-3-22 01:28 作者: Anal-Canal 時間: 2025-3-22 06:13
Carbon and Nitrogen Pools in Terrestrial Ecosystems,on is constantly being absorbed, released, and recycled by a range of natural and human-induced biological and chemical processes. Of fundamental importance is the process of photosynthesis in which plants absorb atmospheric carbon as they grow and convert it to biomass. When plant residues and root作者: Banister 時間: 2025-3-22 09:18
Carbon and Nitrogen Cycles in Terrestrial Ecosystems,ely studied despite being complicated elemental cycles. In the atmosphere, C is mainly present as CO.. Minor amounts of gaseous C occur as CH., CO and other higher molecular C-containing gases. The most abundant N form in the atmosphere is N2. Other gaseous N forms comprise nitrous (N.O) and nitric 作者: phase-2-enzyme 時間: 2025-3-22 16:19
Soil Organic Matter Characterization,ts look into soil organic matter with different perspective. In the glossary of soil science terms (SSSA, 1997) soil organic matter is defined as the organic fraction of the soil exclusive of undecayed plant and animal residues and is considered synonymous with humus. However, other definitions of S作者: phase-2-enzyme 時間: 2025-3-22 18:14 作者: 潛移默化 時間: 2025-3-23 00:13
Carbon and Nitrogen Transformations in Soils,esses affecting organic matter decomposition and formation. The decomposition process is controlled predominantly by bacteria and fungi. Fauna that graze on microbes such as protozoa, nematodes and earthworms also are involved in the mineralization of C and N. Management strategies that target SOM a作者: 靈敏 時間: 2025-3-23 05:00 作者: 不溶解 時間: 2025-3-23 07:27
Leaching Losses and Groundwater Pollution, varies greatly under different cropping and ecosystems. The unutilized N may accumulate in the soil profile and become a contaminant in streams or ground water. Nitrate drained into surface water bodies, e.g. rivers, lakes, or estuaries, can cause deterioration of surface water quality, resulting i作者: Cardiac 時間: 2025-3-23 11:14
Bidirectional Biosphere-Atmosphere Interactions,rogen (nitrous oxide, N.O and nitric oxide, NO) and the halocarbons (a group of gases containing fluorine, chlorine and bromine), which stem from human activities are bringing about major changes to the global environment. These gases accumulate in the atmosphere and their concentration in the envir作者: Somber 時間: 2025-3-23 17:09
Modeling Carbon and Nitrogen Dynamics in the Soil-Plant-Atmosphere System,l work has been undertaken in the last few years in attempts to quantify the emission of greenhouse gases in terrestrial ecosystems and to identify the key factors that govern them. However, fluxes vary greatly between ecosystems, and are often subject to great spatial and temporal variations, withi作者: 埋葬 時間: 2025-3-23 21:11
https://doi.org/10.1007/978-3-642-55859-7 all life forms, inorganic C and N reservoirs and the links between them. This chapter deals with carbon and nitrogen forms and pools, with special focus on the C and N reservoirs in plant biomass and in soils. Carbon and nitrogen fluxes between the different reservoirs are discussed in Chapter 2.作者: Pastry 時間: 2025-3-24 02:04
https://doi.org/10.1007/978-3-030-25763-7tegral part of enzymes in living tissues, that control the biochemical processes in which carbon is involved, such as photosynthesis and respiration. A large variety of microbes are able to transform N in compounds with different oxidation status and to use the released energy by the changes in redo作者: Neutral-Spine 時間: 2025-3-24 04:56 作者: garrulous 時間: 2025-3-24 09:38 作者: 信任 時間: 2025-3-24 13:38
Nondestructive Compositional AnalysispH, soil texture, soil moisture, soil aeration, soil temperature, and management practices such as tillage and fertility amendments. Vegetation type and associated quality of residue inputs directly affect the availability of nutrients by influencing microbial C and N use efficiency. Plant residues 作者: Predigest 時間: 2025-3-24 15:29
Nondestructive Evaluation of Materials land use and land cover can be important contributors to climate change. Since there is a close relationship between the atmosphere, soils and climate, the global climate change will strongly impact all soil processes (Rosenzweig & Hillel, 1995), particularly carbon and nitrogen dynamics. Most land作者: Limerick 時間: 2025-3-24 20:58
https://doi.org/10.1007/978-1-4471-1995-1proximately 20% of wells in farmland areas, between 2-10 mg L. in 35% of wells, and below 2 mg L. in only 40% of wells (Galloway et al., 2004). Indications of increasing NO.-N concentration in water are also emanating from countries with emerging economies, particularly China. Results of the studies作者: 注入 時間: 2025-3-25 02:30 作者: 連鎖,連串 時間: 2025-3-25 03:48 作者: Picks-Disease 時間: 2025-3-25 11:10 作者: ORBIT 時間: 2025-3-25 12:07 作者: 不安 時間: 2025-3-25 18:21 作者: 遭遇 時間: 2025-3-25 21:27 作者: 暖昧關(guān)系 時間: 2025-3-26 01:54 作者: Crumple 時間: 2025-3-26 06:41
Anthropogenic Activities and Soil Carbon and Nitrogen, land use and land cover can be important contributors to climate change. Since there is a close relationship between the atmosphere, soils and climate, the global climate change will strongly impact all soil processes (Rosenzweig & Hillel, 1995), particularly carbon and nitrogen dynamics. Most land作者: 極少 時間: 2025-3-26 09:51 作者: 不出名 時間: 2025-3-26 14:57
Bidirectional Biosphere-Atmosphere Interactions,from the combustion of fossil fuels, there is also a substantial contribution from land use change, due to biomass burning and increased mineralization of soil organic carbon, following the conversion of forest or native grassland to agriculture. In all terrestrial ecosystems except those with bare 作者: 領(lǐng)先 時間: 2025-3-26 19:07 作者: liposuction 時間: 2025-3-26 21:08 作者: CAMEO 時間: 2025-3-27 04:20 作者: farewell 時間: 2025-3-27 06:23
Carbon and Nitrogen in the Terrestrial Environment978-1-4020-8433-1作者: 改進 時間: 2025-3-27 12:44 作者: 粗魯性質(zhì) 時間: 2025-3-27 16:18
978-1-4020-8432-4Springer Science+Business Media B.V. 2008作者: noxious 時間: 2025-3-27 18:08 作者: DAFT 時間: 2025-3-28 01:42 作者: Overdose 時間: 2025-3-28 06:04
https://doi.org/10.1007/978-3-642-55859-7on is constantly being absorbed, released, and recycled by a range of natural and human-induced biological and chemical processes. Of fundamental importance is the process of photosynthesis in which plants absorb atmospheric carbon as they grow and convert it to biomass. When plant residues and root作者: FACT 時間: 2025-3-28 08:36
https://doi.org/10.1007/978-3-030-25763-7ely studied despite being complicated elemental cycles. In the atmosphere, C is mainly present as CO.. Minor amounts of gaseous C occur as CH., CO and other higher molecular C-containing gases. The most abundant N form in the atmosphere is N2. Other gaseous N forms comprise nitrous (N.O) and nitric 作者: inveigh 時間: 2025-3-28 12:05 作者: panorama 時間: 2025-3-28 16:44
Nondestructive Evaluation of Food Quality not a welldefined universal methodology to characterize soil quality and to define a clear set of indicators (see Parr et al., 1992; Karlen et al., 1997; Shaxson, 1998; Bouma, 2002; Nortcliff, 2002; Schj?nning et al., 2002; Gil-Sotres et al., 2005). For a farmer soil quality may mean sustaining or 作者: 地牢 時間: 2025-3-28 21:19
Nondestructive Compositional Analysisesses affecting organic matter decomposition and formation. The decomposition process is controlled predominantly by bacteria and fungi. Fauna that graze on microbes such as protozoa, nematodes and earthworms also are involved in the mineralization of C and N. Management strategies that target SOM a作者: inculpate 時間: 2025-3-29 02:55
Nondestructive Evaluation of Materialsts are exerted through land use and especially land use changes, which almost certainly change the fluxes between soils and the atmosphere (Bolin & Sukumar, 2000). Land use and land cover are linked to climate in complex ways. Form and intensity of land use influence the constellation of the atmosph作者: Legion 時間: 2025-3-29 06:38
