Relevant bibliographies by topics / Carbon cycling

Contents

  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers
  6. Reports

Academic literature on the topic 'Carbon cycling'

Author: Grafiati
Published: 4 June 2021
Last updated: 10 March 2023

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Journal articles on the topic "Carbon cycling"

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Coble, Paula. "Cycling coloured carbon." Nature Geoscience 1, no. 9 (September 2008): 575–76. http://dx.doi.org/10.1038/ngeo294.

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Deane, Caitlin. "Custom carbon cycling." Nature Chemical Biology 13, no. 1 (January 2017): 1. http://dx.doi.org/10.1038/nchembio.2275.

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Keir, Robin. "Carbon isotopes and carbon cycling." Nature 357, no. 6378 (June 1992): 446. http://dx.doi.org/10.1038/357446a0.

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Johnston, Carol A., Peter Groffman, David D. Breshears, Zoe G. Cardon, William Currie, William Emanuel, Julia Gaudinski, et al. "Carbon cycling in soil." Frontiers in Ecology and the Environment 2, no. 10 (December 2004): 522–28. http://dx.doi.org/10.1890/1540-9295(2004)002[0522:ccis]2.0.co;2.

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Delaney, M. L. "Extinctions and carbon cycling." Nature 337, no. 6202 (January 1989): 18–19. http://dx.doi.org/10.1038/337018a0.

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WILSON, ELIZABETH. "DIAMOND ILLUMINES CARBON CYCLING." Chemical & Engineering News Archive 89, no. 38 (September 19, 2011): 6. http://dx.doi.org/10.1021/cen-v089n038.p006a.

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Luo, Yiqi, Christopher B. Field, and Robert B. Jackson. "Does Nitrogen Constrain Carbon Cycling, or Does Carbon Input Stimulate Nitrogen Cycling?1." Ecology 87, no. 1 (January 2006): 3–4. http://dx.doi.org/10.1890/05-0923.

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Ping, C. L., J. D. Jastrow, M. T. Jorgenson, G. J. Michaelson, and Y. L. Shur. "Permafrost soils and carbon cycling." SOIL 1, no. 1 (February 5, 2015): 147–71. http://dx.doi.org/10.5194/soil-1-147-2015.

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Abstract. Knowledge of soils in the permafrost region has advanced immensely in recent decades, despite the remoteness and inaccessibility of most of the region and the sampling limitations posed by the severe environment. These efforts significantly increased estimates of the amount of organic carbon stored in permafrost-region soils and improved understanding of how pedogenic processes unique to permafrost environments built enormous organic carbon stocks during the Quaternary. This knowledge has also called attention to the importance of permafrost-affected soils to the global carbon cycle and the potential vulnerability of the region's soil organic carbon (SOC) stocks to changing climatic conditions. In this review, we briefly introduce the permafrost characteristics, ice structures, and cryopedogenic processes that shape the development of permafrost-affected soils, and discuss their effects on soil structures and on organic matter distributions within the soil profile. We then examine the quantity of organic carbon stored in permafrost-region soils, as well as the characteristics, intrinsic decomposability, and potential vulnerability of this organic carbon to permafrost thaw under a warming climate. Overall, frozen conditions and cryopedogenic processes, such as cryoturbation, have slowed decomposition and enhanced the sequestration of organic carbon in permafrost-affected soils over millennial timescales. Due to the low temperatures, the organic matter in permafrost soils is often less humified than in more temperate soils, making some portion of this stored organic carbon relatively vulnerable to mineralization upon thawing of permafrost.
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Ping, C. L., J. D. Jastrow, M. T. Jorgenson, G. J. Michaelson, and Y. L. Shur. "Permafrost soils and carbon cycling." SOIL Discussions 1, no. 1 (October 30, 2014): 709–56. http://dx.doi.org/10.5194/soild-1-709-2014.

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Abstract. Knowledge of soils in the permafrost region has advanced immensely in recent decades, despite the remoteness and inaccessibility of most of the region and the sampling limitations posed by the severe environment. These efforts significantly increased estimates of the amount of organic carbon (OC) stored in permafrost-region soils and improved understanding of how pedogenic processes unique to permafrost environments built enormous OC stocks during the Quaternary. This knowledge has also called attention to the importance of permafrost-affected soils to the global C cycle and the potential vulnerability of the region's soil OC stocks to changing climatic conditions. In this review, we briefly introduce the permafrost characteristics, ice structures, and cryopedogenic processes that shape the development of permafrost-affected soils and discuss their effects on soil structures and on organic matter distributions within the soil profile. We then examine the quantity of OC stored in permafrost-region soils, as well as the characteristics, intrinsic decomposability, and potential vulnerability of this OC to permafrost thaw under a warming climate.
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Norby, Richard J. "Carbon cycling in tropical ecosystems." New Phytologist 189, no. 4 (February 3, 2011): 893–94. http://dx.doi.org/10.1111/j.1469-8137.2010.03641.x.

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Dissertations / Theses on the topic "Carbon cycling"

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Dubois, Kristal D. "Carbon cycling in northern temperate lakes." Thesis, University of Ottawa (Canada), 2006. http://hdl.handle.net/10393/29347.

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We present two novel stable isotope methods for measuring lake metabolism and compare the results to traditional techniques. The delta 18O method measures planktonic gross primary production (GPP) from dissolved oxygen concentrations, isotopes and respiration (R) and the delta 13C method measures "whole-lake" GPP and R from dissolved oxygen and carbon concentrations and isotopes. All three methods showed GPP was greater than R over the ice-free season and estimates of GPP were not significantly different. There was also no significant difference in R as measured by bottle incubations and the delta13C method. However, the delta 13C method does not account for inputs of external carbon which will result in underestimation of R and overestimation of GPP. In systems with significant allochthonous carbon inputs, the delta13C method cannot be accurate unless these inputs are accounted for. The delta18O method was used to measure metabolic parameters of twenty-one northern temperate lakes and showed GPP dominated over R during the ice-free season. GPP and R were most strongly correlated with lake temperature, which in turn is a function of the amount of solar radiation received by the lake. Our results imply that it is this solar radiation that drives planktonic gross primary productivity, which in turn drives the majority of planktonic respiration. Variation in dissolved organic carbon only explained 8% of the variation in planktonic R, while variation in planktonic GPP explained approximately 80% of the variation in planktonic R. Despite general autotrophy in the lakes, they were generally oversaturated in CO2 during the ice-free season, on average 252+/-25%. However, we found little evidence to conclude that this was the result of an excess of in situ respiration over production. The magnitude of the annual excess of R over GPP was not sufficient to account for the flux to the atmosphere. Moreover, carbon evasion was not a function of respiratory flux, nor did the isotopic signature of dissolved CO2 in the lakes present evidence of respiration. Groundwater inputs of carbon dioxide represent a plausible source for carbon dioxide oversaturation in some but not all of the lakes sampled.
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Jenkins, Meaghan Edith Biological Earth &amp Environmental Sciences Faculty of Science UNSW. "Carbon cycling in sub-alpine ecosystems." Awarded by:University of New South Wales. Biological, Earth & Environmental Sciences, 2009. http://handle.unsw.edu.au/1959.4/44822.

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The relationship between temperature and soil respiration has been well explored although uncertainties remain. This thesis examined the relationship between temperature and rates of heterotrophic respiration in soils from three adjacent sub-alpine Australian vegetation types; woodland, shrubland and grassland. Temperature sensitivity of soil (Q10) has recently been a hotly debate topic, one side concluding that decomposition of recalcitrant, less labile components of soil organic matter are insensitive to temperature. Whilst others argue that there is no difference in the temperature sensitivities of labile and recalcitrant carbon pools. Robust modeling of rates of soil respiration requires characterization of the temperature response of both labile and recalcitrant pools. Laboratory incubation provides a means of characterizing the temperature response of rates of respiration whilst reducing the confounding effects encountered in the field, such as seasonal fluctuations in temperature, moisture and substrate supply. I used a novel system that allowed laboratory measurement of gas exchange in soils over a range of temperatures under controlled conditions. Measurements included CO2 efflux and O2 uptake over a range of temperatures from 5 to 40oC, characterization of temperature response and sensitivity, and respiratory quotients. Rates of heterotrophic respiration fitted both exponential and Arrhenius functions and temperature sensitivity varied and depended on the model used, vegetation type and depth in the soil profile. Long-term incubation indicated both labile and resistant pools of carbon had similar temperature sensitivities. Respiratory quotients provided a strongly predictive measure of the potential rate of decomposition of soil C, independent of the temperature response of respiration, providing a tool that may be used alongside derived parameters to help understand shifts in microbial use of C substrates. Vegetation type influenced soil chemical properties and rates of heterotrophic respiration. Rates of respiration correlated well with concentrations of carbon and nitrogen as has been previously observed, unlike previous studies however a positive correlation was observed between indices of plant available phosphorus and respiration. The soils examined were from three adjacent vegetation types formed on common geology, I concluded that vegetation type had a significant influence on soil, in contrast to the commonly held view by ecologists that soil type drives patterns in vegetation. Climatic effects such as longer, dryer hotter summer, reduced snow cover and increased incidence of extreme weather events such as frosts and bushfire are likely to drive patterns in vegetation in this region and therefore have a significant impact on carbon cycling in Sub-alpine Australian soils.
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Burns, Rebecca Kate. "Cryogenic carbon cycling at an Icelandic glacier." Thesis, Lancaster University, 2016. http://eprints.lancs.ac.uk/85961/.

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Glaciers and ice caps are recognised as an important component of the global carbon cycle. Carbon within glacial systems exists in organic and inorganic forms, across supraglacial, englacial and subglacial realms. It is often difficult to detach cryospheric carbon cycling from hydrology, with the transfer of carbon between glacial inventories relying upon meltwater flows. Classical glacial hydrology consists of distributed drainage delivering delayed flow meltwaters, throughout the accumulation season, superseded by quick flow, aerated channelized drainage during increased ablation. It is upon this template that most existing studies have addressed the dynamics of carbon within glaciated catchments. However, Icelandic glacial systems provide an opportunity to investigate the role of subglacial volcanism in driving carbon dynamics. Hydrochemical properties of Sόlheimajökull bulk meltwaters indicate untraditional redox conditions, with discharge of reduced, anoxic meltwaters in Summer, when expansion of subglacial drainage intersects the Katla geothermal zone. This unique hydrological regime generates profound effects upon the solute flux from the glacier, particularly with regard to the carbon budget. Dissolved inorganic carbon dynamics are dominated by weathering of basaltic bedrocks and accessory hydrothermal calcites, fuelled by subglacial geothermal proton supply. Widespread basal anoxia during summer facilitates methanogenesis resulting in large quantities of methane being discharged from beneath the glacier (flux range between 9,179 to 22,551 tonnes per year). Evidence suggests subglacial microbial acetoclastic methanogenesis is responsible with δ13C and δD CH4 values of ~60‰ and -320‰ respectively, supported by laboratory identification of methanogenesis in Sόlheimajökull subglacial sediments. The organic counterpart to the carbon cycle is invoked to serve as the energy source for microbial metabolism. Such direct measurements of subglacial methane have rarely been achieved at contemporary ice margins. This study therefore provides an exciting opportunity to identify methane sources and carbon cycling in areas subjected to subglacial volcanism and to consider these within the broader context of global carbon dynamics.
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Ludwig, Rebecca. "Carbon cycling and calcification in hypersaline microbial mats." [S.l.] : [s.n.], 2004. http://deposit.ddb.de/cgi-bin/dokserv?idn=979757312.

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Cleary, Meagan B. "Carbon cycling dynamics during succession in sagebrush steppe." Laramie, Wyo. : University of Wyoming, 2007. http://proquest.umi.com/pqdweb?did=1362520811&sid=3&Fmt=2&clientId=18949&RQT=309&VName=PQD.

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Littler, K. "Climate and carbon-cycling in the Early Cretaceous." Thesis, University College London (University of London), 2011. http://discovery.ucl.ac.uk/1335899/.

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The Cretaceous (~145–65 Ma) is widely regarded as a greenhouse period with warm, equable climates and elevated atmospheric CO2 relative to the modern. However, the earliest Cretaceous (Berriasian–Barremian; 145–125 Ma) is commonly characterised as a relatively colder “coolhouse” interval, typified by lower global temperatures than the mid-Cretaceous. Unfortunately, the lack of absolute sea surface temperature (SST) estimates prior to the Barremian has hampered efforts to definitively reconstruct Early Cretacous climate. Here, the TEX86 palaeotemperature proxy, for which a detailed review is provided, has been used to generate a 13 myr record of SST estimates for the Early Cretaceous, based on sediments from assorted deep-sea drilling sites. A consistent offset in the TEX86 ratio between transported mudstones and pelagic carbonates in the low-latitude marine sediments (DSDP Sites 603 and 534) has been identified, which may be linked to post-burial diagenesis or a difference in organic matter type between lithologies. Mindful of these apparent lithological effects on TEX86, only the pelagic sediments were used to subsequently reconstruct Early Cretaceous SSTs. These TEX86 records demonstrate both elevated SSTs (>27 ºC) at low and mid-latitudes relative to the modern, and the apparent stability of these high temperatures over long timescales. This lack of SST variation in the low-latitudes during the Valanginian positive carbon-isotope event (CIE; ~135–138 Ma), casts doubt on the warming-weathering feedback model put forward to explain this major perturbation. Additionally, new paired bulk organic (δ13Corg) and bulk carbonate (δ13Ccarb) carbon-isotope records from North Atlantic DSDP sites, have been used to reconstruct relative changes in pCO2 across the CIE. These observed fluctuations in Δ13C imply changes in carbon-cycling and a possible drawdown in CO2, due to excess organic matter burial associated with the CIE.
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Whisner, Carla. "Inorganic carbon cycling in agricultural lands, Coshocton, Ohio." Connect to resource, 2009. http://hdl.handle.net/1811/37273.

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Bowers, Samuel Jonathan. "Fire dynamics and carbon cycling in miombo woodlands." Thesis, University of Edinburgh, 2017. http://hdl.handle.net/1842/28804.

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Savannah ecosystems play a prominent role in the global carbon (C) cycle, yet fluxes are poorly quantified, and the key processes regulating vegetation dynamics are uncertain. Insight is particularly deficient in southern Africa’s miombo woodlands, a woody savannah that is home to over 100 million people. This biome is heavily disturbed, with widespread deforestation and degradation associated with agriculture, charcoal and timber extraction, and frequent fires from anthropogenic sources. In this thesis I combine plot inventory data with remote sensing and modelling techniques to improve our understanding of the miombo woodland C cycle. Using a network of forest inventory plots, I characterise floristic and functional diversity in a savannah-forest mosaic in southeastern Tanzania. Divergent vegetation structures are associated with variation in fire frequency, water supply, and soil chemo-physical properties. Corresponding differences are noted in fire resilience, water-use, and nutrient acquisition plant functional traits, suggesting that multiple interrelated environmental filters act to assemble heterogeneous tree communities. Re-inventory of forest plots was used to quantify key aspects of the woody C cycle. Tree growth rates are slow, calling for careful management of woodland resources, and significantly reduced where stems were damaged. Stem mortality is rare, though elevated in the smallest trees and where damage was recorded. Contemporary strategies to incentivise the conservation of miombo woodland ecosystems, such as the REDD+ programme of the United Nations, advocate payments for sustaining ecosystem services such as C sequestration. I report on a pilot REDD+ project aiming to reduce woodland degradation from frequent high intensity fires in southeastern Tanzania. Model simulations suggest that woody biomass is being gradually lost from the region, and that setting early season fires has the potential to reverse this trend. Realising substantial changes in C storage requires a demanding reduction to late fire frequency, and uncertainty in model predictions remains high. I quantify the C cycle of southern African woodlands by combining observational data with a diagnostic C cycle model under a model-data fusion framework. Model outputs show substantial variation in primary production, C allocation patterns, and foliar and canopy traits, which are associated with differences in woody cover, fire, and precipitation properties. C cycle dynamics correspond poorly to conventional land cover maps, indicating they may be unsuited to upscaling measurements and models of the terrestrial C cycle.
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Blount, Keyyana. "Land Use Effects on Carbon Cycling in Oregon Coastal Wetlands." Thesis, University of Oregon, 2018. http://hdl.handle.net/1794/23152.

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Pacific Northwest coastal wetland extent has been significantly reduced due to development. To understand the effects of land use change on carbon cycling in coastal wetlands, we compared soil carbon dynamics in restored, disturbed (by diking or draining), and reference wetlands in both freshwater and saline conditions in Coos Bay, Oregon. We quantified soil carbon pools, measured in situ fluxes of methane (CH4) and carbon dioxide (CO2), and estimated sediment deposition and carbon sequestration rates. We found that land use change influences carbon cycling and storage in coastal wetlands. The disturbed marshes have likely lost all their organic material after draining or diking, except for a shallow A horizon. The restored marsh in situ CH4 and CO2 fluxes were intermediate between the disturbed and reference marshes. Generally, restored marshes showed a partial return of carbon storage functions, or an indication that reference level functions may be achieved over time.
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Dixon, Simon David. "Controls on carbon cycling in upland blanket peat soils." Thesis, Durham University, 2012. http://etheses.dur.ac.uk/3641/.

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Peatlands are a globally important, terrestrial store of carbon and the UK is recognised as an internationally significant holder of peatlands. Of all the kinds of peatland found in the UK, blanket bogs are dominant, representing 87% of the UK’s peatland area. The UK’s peatlands, in contrast to many other areas of boreal/temperate peat, are relatively accessible and as such have been subject to land-management pressures for many thousands of years. These management pressures have led to the deterioration of many peatlands in the UK, with only 1% of England’s peatlands being considered ‘pristine’ in a Natural England report (Natural England, 2010). Climate change and increasing land-use pressures are predicted to affect all UK peatlands in coming years. As such, studies of the drivers of carbon cycling on UK peatlands are being undertaken in order to help in the construction of models to predict the dynamics of peatland carbon balance. These models will subsequently enable land-managers and policy makers to take informed decisions regarding peatland management and carbon storage. One such model of peatland carbon balance is the Durham Carbon Model, which uses a mass balance between fluxes of carbon in and out of a peatland in order to estimate its net carbon budget. While the Durham Carbon Model is able to deal with the effects of some aspects of land-management on peatland carbon balance, there remain a number of important drivers as yet unaccounted for in the model. As such, the remit of this thesis was to conduct in-situ, experiments in order to provide additional data on peatland carbon cycling with a view to incorporating these drivers into the model. Specifically, this research examines three areas as yet unaccounted for in the Durham Carbon Model: altitude, vegetation and diurnal processes. These factors are considered relative to CO2 flux and, in some cases, soil pore water dissolved organic carbon concentration. Additional experiments were also performed to determine whether empirical models of CO2 flux can be physically interpretable. Results obtained for this thesis suggest that the most important factor in predicting CO2 flux on blanket peat soils is vegetation type and vegetation mediated processes, i.e. photosynthetic controls on respiration. Moreover, the relationship between respiration and photosynthesis was found across a range of other factors and temporal scales. In addition to vegetation, altitude was found to significantly affect CO2 for some vegetation types. Therefore, both of these factors are to be incorporated into the Durham Carbon Model. Experiments suggested that empirical models of CO2 flux can be physically interpretable. The results of the diurnal experiment gave evidence to support the hypothesis that some component of the relationship between photosynthesis and respiration is temporally lagged, perhaps by 3 hours. However, the results were not unequivocal and thus further work is needed to fully examine some of the results presented herein.
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Books on the topic "Carbon cycling"

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Baird, Andrew J., Lisa R. Belyea, Xavier Comas, A. S. Reeve, and Lee D. Slater, eds. Carbon Cycling in Northern Peatlands. Washington, D. C.: American Geophysical Union, 2009. http://dx.doi.org/10.1029/gm184.

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1969-, Baird Andrew J., ed. Carbon cycling in northern peatlands. Washington, DC: American Geophysical Union, 2009.

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1969-, Baird Andrew I., ed. Carbon cycling in northern peatlands. Washington, DC: American Geophysical Union, 2009.

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1969-, Baird Andrew J., ed. Carbon cycling in northern peatlands. Washington, DC: American Geophysical Union, 2009.

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Datta, Rahul, Ram Swaroop Meena, Shamina Imran Pathan, and Maria Teresa Ceccherini, eds. Carbon and Nitrogen Cycling in Soil. Singapore: Springer Singapore, 2020. http://dx.doi.org/10.1007/978-981-13-7264-3.

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Kulinski, Karol, and Janusz Pempkowiak. Carbon Cycling in the Baltic Sea. Berlin, Heidelberg: Springer Berlin Heidelberg, 2012. http://dx.doi.org/10.1007/978-3-642-19388-0.

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Kulinski, Karol. Carbon Cycling in the Baltic Sea. Berlin, Heidelberg: Springer Berlin Heidelberg, 2012.

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1968-, Zhang Chuanlun, ed. Microbial processes and carbon cycling in the ocean. New York: Nova Science Pub., 2008.

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Schulze, Ernst-Detlef, ed. Carbon and Nitrogen Cycling in European Forest Ecosystems. Berlin, Heidelberg: Springer Berlin Heidelberg, 2000. http://dx.doi.org/10.1007/978-3-642-57219-7.

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Sveriges lantbruksuniversitet. Institutionen fo r ekologi och miljo va rd., ed. Theoretical analyses of C and N cycling in soil. Uppsala: Swedish University of Agricultural Sciences, Dept. of Ecology and Environmental Research, 1987.

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Book chapters on the topic "Carbon cycling"

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Hardison, Amber K., and Elizabeth A. Canuel. "Carbon (Organic, Cycling)." In Encyclopedia of Geobiology, 230–34. Dordrecht: Springer Netherlands, 2011. http://dx.doi.org/10.1007/978-1-4020-9212-1_45.

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Jennings, Gail. "Cycling for Change? Exploring the Role of Carbon Consciousness Among Cape Town’s Intentional Cyclists." In Cycling Societies, 219–38. Abingdon, Oxon ; New York, NY : Routledge, 2021. | Series: Routledge studies in transport, environment and development: Routledge, 2020. http://dx.doi.org/10.4324/9780429321092-17.

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Kuliński, Karol, and Janusz Pempkowiak. "Climate and Carbon Cycle." In Carbon Cycling in the Baltic Sea, 5–47. Berlin, Heidelberg: Springer Berlin Heidelberg, 2012. http://dx.doi.org/10.1007/978-3-642-19388-0_2.

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Cerri, Carlos Clemente, Martial Bernoux, Brigitte Josefine Feigl, and Carlos Eduardo Pellegrino Cerri. "Carbon Cycling in the Amazon." In Recarbonization of the Biosphere, 253–73. Dordrecht: Springer Netherlands, 2012. http://dx.doi.org/10.1007/978-94-007-4159-1_12.

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Kim, Il-Nam, Kitack Lee, and Jeomshik Hwang. "Natural and Anthropogenic Carbon Cycling." In Oceanography of the East Sea (Japan Sea), 169–89. Cham: Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-22720-7_7.

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Vishnivetskaya, Tatiana A., Susanne Liebner, Roland Wilhelm, and Dirk Wagner. "Microbial Carbon Cycling in Permafrost." In Polar Microbiology, 181–99. Washington, DC, USA: ASM Press, 2014. http://dx.doi.org/10.1128/9781555817183.ch9.

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Holden, J., R. P. Smart, P. J. Chapman, A. J. Baird, and M. F. Billett. "The Role of Natural Soil Pipes in Water and Carbon Transfer in and from Peatlands." In Carbon Cycling in Northern Peatlands, 251–64. Washington, D. C.: American Geophysical Union, 2013. http://dx.doi.org/10.1029/2008gm000804.

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Tokida, Takeshi, Tsuyoshi Miyazaki, and Masaru Mizoguchi. "Physical Controls on Ebullition Losses of Methane from Peatlands." In Carbon Cycling in Northern Peatlands, 219–28. Washington, D. C.: American Geophysical Union, 2013. http://dx.doi.org/10.1029/2008gm000805.

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Artz, Rebekka R. E. "Microbial Community Structure and Carbon Substrate use in Northern Peatlands." In Carbon Cycling in Northern Peatlands, 111–29. Washington, D. C.: American Geophysical Union, 2013. http://dx.doi.org/10.1029/2008gm000806.

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Laine, Jukka, Kari Minkkinen, and Carl Trettin. "Direct Human Impacts on the Peatland Carbon Sink." In Carbon Cycling in Northern Peatlands, 71–78. Washington, D. C.: American Geophysical Union, 2013. http://dx.doi.org/10.1029/2008gm000808.

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Conference papers on the topic "Carbon cycling"

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ZHUANG, YA-HUI, HONG-XUN ZHANG, and CHANGSHENG LI. "Sustainable Carbon Cycling." In Proceedings of the Third Asia-Pacific Conference. WORLD SCIENTIFIC, 2000. http://dx.doi.org/10.1142/9789812791924_0004.

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Jaworske, Donald. "Thermal Cycling of Thermal Control Paints on Carbon-Carbon and Carbon-Polyimide Composites." In 3rd International Energy Conversion Engineering Conference. Reston, Virigina: American Institute of Aeronautics and Astronautics, 2005. http://dx.doi.org/10.2514/6.2005-5589.

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Brown, Grace, Ben Brock, Paul Mann, and Stuart Dunning. "CARBON GAS CYCLING IN SUPRAGLACIAL DEBRIS COVERS." In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-357190.

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Rezanezhad, Fereidoun, Arash Rafat, Eunji Byun, William Quinton, Elyn Humphreys, Kara Webster, and Philippe Van Cappellen. "Peatlands and Climate Warming: Winter Carbon Cycling." In Goldschmidt2022. France: European Association of Geochemistry, 2022. http://dx.doi.org/10.46427/gold2022.12141.

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Nwokoro, Chinedu E. C., Clare Ewin, Clare Harrison, Mubin Ibrahim, Isobel Dundas, Iain Dickson, Naseem Mushtaq, and Jonathan Grigg. "Urban Cycling And Black Carbon In Airway Macrophages." In American Thoracic Society 2012 International Conference, May 18-23, 2012 • San Francisco, California. American Thoracic Society, 2012. http://dx.doi.org/10.1164/ajrccm-conference.2012.185.1_meetingabstracts.a1729.

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"A minimalistic model for carbon cycling in wetlands." In 19th International Congress on Modelling and Simulation. Modelling and Simulation Society of Australia and New Zealand (MSSANZ), Inc., 2011. http://dx.doi.org/10.36334/modsim.2011.e11.coletti.

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Eguchi, James, Charles W. Diamond, and Timothy Lyons. "PROTEROZOIC OXYGENATIONS AND CARBON ISOTOPE EXCURSIONS DRIVEN BY COUPLED SURFACE-INTERIOR CARBON CYCLING." In GSA Connects 2021 in Portland, Oregon. Geological Society of America, 2021. http://dx.doi.org/10.1130/abs/2021am-369606.

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Lee, Cin-Ty. "Carbon cycling from source to sink in magmatic orogens." In Goldschmidt2021. France: European Association of Geochemistry, 2021. http://dx.doi.org/10.7185/gold2021.6612.

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Li, Min, Wei Zhang, Chaosheng Wang, and Huaping Wang. "Fabrication of Conductive Porous Structure Loaded With Carbon Black and/or Carbon Nanotube." In ASME 2011 International Mechanical Engineering Congress and Exposition. ASMEDC, 2011. http://dx.doi.org/10.1115/imece2011-65122.

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Abstract:
Carbon black (CB) and/or carbon nanotube (CNT) loaded porous PP frame with enhanced conductivity was facilely fabricated via immiscible co-continuous polymer blend and subsequent dissolution process. The SEM result indicated that the agglomerated carbon additives formed continuous phase on the inner wall of the interconnected micro channel. Nitrogen gas adsorption test was carried out to characterize the nano pores resulted from these nano particles. In addition, the electrochemical performance of the material was evaluated by cyclic voltammetry and galvanostatic charge-discharge cycling. Experimental results demonstrate the effectiveness of this novel method to construct conductive material with hierarchical porous structure which integrates co-continuous porous structure with nano pores derived from deposited carbon additives.
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Inose, Takashi, Tomoko Ogura Iwasaki, Sheyang Ning, Darlene Viviani, Monte Manning, X. M. Henry Huang, Thomas Rueckes, and Ken Takeuchi. "Reliability study of Carbon Nanotube memory after various cycling conditions." In 2016 IEEE Silicon Nanoelectronics Workshop (SNW). IEEE, 2016. http://dx.doi.org/10.1109/snw.2016.7577997.

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Reports on the topic "Carbon cycling"

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Das, K. C., Adams, T. Thomas, Mark A. Eiteman, James R. Kastner, Sudhagar Mani, and Ryan Adolphson. Biorefinery and Carbon Cycling Research Project. Office of Scientific and Technical Information (OSTI), June 2012. http://dx.doi.org/10.2172/1053782.

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Alexandra Hedgpeth, Alexandra Hedgpeth. Carbon in Arctic Permafrost : An incubation experiment looking at carbon cycling. Experiment, November 2014. http://dx.doi.org/10.18258/4001.

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Bogner, J., and A. Lagerkvist. Organic carbon cycling in landfills: Model for a continuum approach. Office of Scientific and Technical Information (OSTI), September 1997. http://dx.doi.org/10.2172/555441.

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House, Geoffrey Lehman, Laverne A. Gallegos-Graves, and Patrick Sam Guy Chain. Overview of the Soil Metagenomics and Carbon Cycling SFA Fungal Collection. Office of Scientific and Technical Information (OSTI), November 2018. http://dx.doi.org/10.2172/1483488.

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Myrold, David D., Peter J. Bottomely, Ari Jumpponen, Charles W. Rice, Lydia H. Zeglin, Maude M. David, Janet K. Jansson, Emmanuel Prestat, and Robert L. Hettich. Unveiling Microbial Carbon Cycling Processes in Key U.S. Soils using ''Omics''. Office of Scientific and Technical Information (OSTI), September 2014. http://dx.doi.org/10.2172/1156887.

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Coble, Paula. Distribution and Cycling of Dissolved Organic Carbon and Colored Dissolved Organic Carbon on the West Florida Shelf. Fort Belvoir, VA: Defense Technical Information Center, August 2002. http://dx.doi.org/10.21236/ada628308.

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Coble, Paula. Distribution and Cycling of Dissolved Organic Carbon and Colored Dissolved Organic Carbon on the West Florida Shelf. Fort Belvoir, VA: Defense Technical Information Center, September 2007. http://dx.doi.org/10.21236/ada573071.

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Monson, Russell K. Carbon Cycling Dynamics in Response to Pine Beetle Infection and Climate Variation. Office of Scientific and Technical Information (OSTI), January 2015. http://dx.doi.org/10.2172/1168588.

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Maher, Katharine, and Jennifer Druhan. A multiscale approach to modeling carbon cycling within a high-elevation watershed. Office of Scientific and Technical Information (OSTI), March 2019. http://dx.doi.org/10.2172/1502944.

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Chamberlain, Morgan, Justin Miller, Diana Heflin, Teal Dowd, Jung Soo Rhim, Ilke Arturk, Jacob Coffing, and Jan-Anders Mansson. Cycling and Sustainability: Development of a Recycled Carbon Fiber (rCF) Crankset Demonstrator. Purdue University, 2022. http://dx.doi.org/10.5703/1288284317532.

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You might also be interested in the extended bibliographies on the topic 'Carbon cycling' for particular source types:
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