Relevant bibliographies by topics / Dissolved organic carbon

Academic literature on the topic 'Dissolved organic carbon'

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Published: 4 June 2021
Last updated: 1 June 2024

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Journal articles on the topic "Dissolved organic carbon"

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Gonet, S. S., and B. Debska. "Dissolved organic carbon and dissolved nitrogen in soil under different fertilization treatments." Plant, Soil and Environment 52, No. 2 (November 15, 2011): 55–63. http://dx.doi.org/10.17221/3346-pse.

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The objective of the study was to evaluate the effects of long-term fertilization of a sandy soil with differentiated doses of cattle slurry as well as its after-effect action on the possibilities of migration of dissolved organic carbon (DOC) and dissolved nitrogen (DNt) down to deeper layers of the soil profile. DOC and DNt were extracted with borate buffer and 0.004M CaCl<sub>2</sub> solution. Evaluation of effects of cattle slurry on the content of DOC and DNt was done in comparison with mineral fertilization. It was shown that the use of cattle slurry in the doses of 100 and 200&nbsp;m<sup>3</sup>/ha caused a significant increase of labile organic matter in the 0&ndash;25 and 25&ndash;50 cm layers of soil. As compared with mineral fertilization the application of slurry increased also the amounts of extracted DNt, but only in the surface layer. The DNt content in the deeper soil horizons did not depend on the kind of fertilization. Concentrations of DOC and DNt in the extracts depended not only on their content in soil but it was also modified substantially by the extractant used.
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Remeš, M., and J. Kulhavý. "Dissolved organic carbon concentrations under conditions of different forestcomposition." Journal of Forest Science 55, No. 5 (April 20, 2009): 201–7. http://dx.doi.org/10.17221/16/2009-jfs.

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The study deals with the monitoring of dissolved organic carbon (DOC) concentrations in seepage water sampled from differently managed forest plots in the Drahanská vrchovina Upland. Simultaneously, the input of DOC in precipitation and throughfall is evaluated. Preliminary results show higher mobility level of carbon substances in forest soil in a pure spruce stand compared to mixed stand or a pure beech stand. DOC can be one of suitable characteristics to evaluate the conversion effectiveness of spruce monocultures.
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Meyer, Judy L. "Dissolved organic carbon dynamics in two subtropical blackwater rivers." Archiv für Hydrobiologie 108, no. 1 (November 25, 1986): 119–34. http://dx.doi.org/10.1127/archiv-hydrobiol/108/1986/119.

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Robarts, Richard D., and Peter J. Ashton. "Dissolved organic carbon and microbial activity in a hypertrophic African reservoir." Archiv für Hydrobiologie 113, no. 4 (November 7, 1988): 519–39. http://dx.doi.org/10.1127/archiv-hydrobiol/113/1988/519.

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Hansell, Dennis A. "Recalcitrant Dissolved Organic Carbon Fractions." Annual Review of Marine Science 5, no. 1 (January 3, 2013): 421–45. http://dx.doi.org/10.1146/annurev-marine-120710-100757.

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Rochelle-Newall, E. J., and T. R. Fisher. "Chromophoric dissolved organic matter and dissolved organic carbon in Chesapeake Bay." Marine Chemistry 77, no. 1 (January 2002): 23–41. http://dx.doi.org/10.1016/s0304-4203(01)00073-1.

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Tian, Xiaokang, and Siyue Li. "Quality and Biodegradation Process of Dissolved Organic Carbon in Typical Fresh-Leaf Leachate in the Wuhan Urban Forest Park." Water 16, no. 4 (February 12, 2024): 558. http://dx.doi.org/10.3390/w16040558.

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The study investigated the leaching and biodegradation of dissolved organic carbon in leaf leachates from typical fresh leaves in the Wuhan Urban Forest Park, Central China. The fresh leaf-leached dissolved organic carbon quality and biodegradability, as well as their potential determinants, were examined for 12 major tree species, including deciduous trees and shrubs. A 28-day indoor incubation was conducted at two temperature conditions of 20 °C and 30 °C. Sampling was conducted within the planned time frame for experimental measurements, and a first-order kinetic model for dissolved organic carbon degradation was fitted. The utilization of the fir tree as the predominant deciduous species and cuckoo as the primary shrubs provided advantages in increasing the carbon sequestration capacity of urban forests. There was no significant difference in the degradation rate of the leaching solution at different temperatures, but the k value of the first-order kinetic model was different. At 20 °C, the dissolved organic carbon degradation rate was positively correlated with electrical conductivity and total dissolved nitrogen, while it was negatively correlated with the humification index and ratio of dissolved organic carbon to total dissolved nitrogen. At 30 °C, the degradation rate of dissolved organic carbon showed a positive correlation with total dissolved phosphorus and total dissolved nitrogen, while it was negatively correlated with the humification index, ratio of dissolved organic carbon to total dissolved nitrogen and ratio of dissolved organic carbon to total dissolved phosphorus.
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Sketchell, Joanne, Hans G. Peterson, and Nick Christofi. "Dissolved Organic Carbon Removal from a Prairie Water Supply Using Ozonation and Biological Activated Carbon." Water Quality Research Journal 34, no. 4 (November 1, 1999): 615–32. http://dx.doi.org/10.2166/wqrj.1999.032.

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Abstract Large quantities of dissolved organic carbon in prairie surface water reservoirs make sustainable treatment quite challenging. Organic material is a precursor for the formation of disinfection by-products. Here, ozonation and biological activated carbon filtration were used as methods for removing dissolved organic carbon from the water of a small prairie reservoir used as a drinking water source. Biofiltration alone yielded significant reductions in dissolved organic carbon, colour, total trihalomethanes and chlorine demand. When ozonation preceded biofiltration, the increased proportion of biodegradable dissolved organic carbon allowed for significantly greater (p&lt;0.05
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Escobar, Isabel C., and Andrew A. Randall. "Assimilable organic carbon (AOC) and biodegradable dissolved organic carbon (BDOC):." Water Research 35, no. 18 (December 2001): 4444–54. http://dx.doi.org/10.1016/s0043-1354(01)00173-7.

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McCracken, Kimberly L., William H. McDowell, Robert D. Harter, and Christine V. Evans. "Dissolved Organic Carbon Retention in Soils." Soil Science Society of America Journal 66, no. 2 (2002): 563. http://dx.doi.org/10.2136/sssaj2002.0563.

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Dissertations / Theses on the topic "Dissolved organic carbon"

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Zhang, Zhuoli. "Dissolved organic carbon (DOC) management in peatlands." Thesis, Durham University, 2015. http://etheses.dur.ac.uk/11357/.

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Peatlands are serving as one of the most important terrestrial carbon stores in the United Kingdom and globally. In the UK, the current trend of peatlands turning from carbon sinks to carbon sources is widely observed and reported. As numerous factors may affect the carbon cycle of peatlands, including climate, land management, hydrology and vegetation, dissolved organic carbon (DOC) was commonly used as an indicator of peatland carbon changes. Besides the function as an indicator of carbon turnover in peatland, increasing DOC in the stream water also raises concern in water companies as the removal of DOC from water represents a major cost of water treatment. This thesis investigates the impacts of land management such as drain blocking and revegetation on stream DOC changes. By building a pilot column study, this thesis also assessed the potential of bank filtration serving as DOC treatment in UK. Results of drain blocking shows the management was a significant impact on the DOC changes. However, later investigation of peak flow events indicates such positive impacts from drain blocking were minor in terms of high peak flow events. Since the majority of DOC export occurred during such peak flow events, drain blocking were found not as an efficient management of DOC changes. The field study of revegetation observed minor effects of revegetation on stream DOC. The results of column bank filtration indicate low DOC removal rate under the current stream DOC level in UK. The bank filtration may efficient remove DOC when higher DOC input applied. However, it is not suitable for UK peatland under current DOC export.
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Pan, Xi. "The marine biogeochemistry of dissolved organic carbon and dissolved organic nutrients in the Atlantic Ocean." Thesis, University of Southampton, 2007. https://eprints.soton.ac.uk/63139/.

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The marine biogeochemistry of dissolved organic carbon (DOC) has come under increased scrutiny because of its involvement in the global carbon cycle and consequently climate change. Dissolved organic nitrogen (DON) and phosphorus (DOP), which have historically been ignored because of their suggested “biological unavailability”, have now received greater attention due to their importance in nutrient cycling, particularly in oligotrophic ecosystems. DOM, a byproduct of photosynthetic production, has important ecological significance as a substrate that supports heterotrophic bacterial growth, thereby causing oxygen consumption and regenerating inorganic nutrients. In the open ocean the net production of DOC is ultimately due to the decoupling of biological production and consumption processes. Concentrations of DOM in the surface oceans, therefore, are controlled by both physical and biological processes. This research investigates the biological factors that control the distributions of DOC, DON and DOP in surface waters, the importance of DOC degradation to oxygen consumption, the importance of DON and DOP degradation to remineralised dissolved inorganic nitrogen (DIN) and dissolved inorganic phosphorus (DIP), and the C:N:P stoichiometry of DOM pool in the Atlantic Ocean. Samples were collected on Atlantic Meridional Transects (AMT) cruise 16 and 17, which crossed the southern temperate region, the southern subtropical gyre, the equatorial region, the northern subtropical gyre, and the northern temperate region. This work described here was performed as a component of the AMT programme. Concentrations of DOC and TDN were determined using a high-temperature catalytic combustion technique, and TDP concentrations were determined using a UV oxidation method. Concentrations of DON and DOP were estimated as the difference between the independent measurements of TDN and TDP. The results showed that the highest DOM concentrations were found in surface (0-30 m) waters, ranging from 70-80 µM DOC, 4.8-6.5 µM DON and 0.2-0.3 µM DOP, and decreased with increasing water depth to 45-55 µM DOC, 2.6-4.0 µM DON and 0.04-0.05 µM DOP at 300 m. The lowest DOM concentrations were observed in the deep (>1000 m) ocean, averaging 44 µM DOC, 2.3 µM DON and 0.02 µM DOP. In the upper 300 m, the concentrations of semilabile (and labile) DOC decreased by 45-95% from the surface values. DON and DOP were the dominant components of the total dissolved nutrient pools in the upper 50 m, accounting for up to 99% and 80% of the TDN and TDP pools, respectively. In the upper 300 m, semilabile (and labile) DON and DOP decreased by 50-65% and 90-95% from the surface values, respectively. The decoupled correlations between DOC/DON/DOP and chlorophyll-a and rates of carbon fixation suggested that phytoplankton biomass and rates of primary production were not the important controls of the cumulative DOC, DON and DOP. Zooplankton grazing was hypothesised to be an important factor in regulating the distributions of DOC, DON and DOP in surface waters. Poor correlations between DOC/DON/DOP and DIN/DIP suggested that inorganic nutrients were not the significant controls in DOC, DON and DOP distributions. N and P were probably retained mainly in the organic pool in the surface waters due to a hypothesised insufficient functioning of the microbial degradation. If the vertical migration of zooplankton was significant in bringing new nutrients into the surface waters, strong correlations between dissolved organic and inorganic nutrients should not be anticipated. Prochlorococcus spp. abundance was statistically linked with the concentrations of DOC, DON and DOP. The significant correlations may reflect the ability of Prochlorococcus to assimilate the labile forms of dissolved organic nutrients (including DOC), which may be quantitatively significant in surface waters of the Atlantic Ocean. The C:N, N:P and C:P stoichiometry of the bulk DOM pool deviated from the Redfield ratio of 6:1, 16:1 and 106:1, ranging from 12-18, 20-100 and 300-1400, respectively, in the upper 300 m, suggesting that the cumulative DOM was rich in C relative to N and P, and N relative to P compared to the Redfield trajectories. The offsets of the C:N:P stoichiometry relatively to the Redfield ratio were due to nutrient limitations that imposed on prokaryotic and eukaryotic microbial populations. The C:N:P stoichiometry of the bulk DOM pool showed an increased trend, with C:N = 12-16, N:P = 20-25, and C:P = 300-350 in the upper 30 m, C:N = 12-18, N:P = 50-100, and C:P = 700-1400 at 300 m, and C:N = 17-24, N:P = 79-132; C:P = 1791-2442 at 1000 m. The differences in the C:N:P stoichiometry of the bulk DOM pool between the upper and deep waters suggested preferential remineralisation of P relative to C and N, and N relative to C. A greater remineralisation length scale for DOC relative to DON and DOP produced a long-term, steady flux of C from the surface to the deep ocean. Therefore, CO2 fixed in the upper ocean during planktonic photosynthesis was continuously “pumped” into the ocean interior, and stored in the deep ocean up to thousands of years. The C:N, N:P and C:P stoichiometry of the semilabile (and labile) DOM pool generally agreed with the Redfield ratio (C:N = 6; N:P = 16; C:P = 106) in the upper 30 m. At 100 m C:N ratio was 5-12, C:P ratio was 20-30, and C:P ratio was 100-150. At 300 m, C:N ratio was 5-12, N:P ratio was 25-100, and C:P ratio was 150-500. The findings suggested that in the upper 300 m, there was no preferential remineralisation between the semilabile (and labile) DOC and DON, however, the semilabile (and labile) DOP seemed to be preferentially remineralised relative to the semilabile (and labile) DOC and DON. In the upper thermocline (i.e. above 300 m), DOC degradation was important with respect to oxygen consumption, contributing to as much as 25% of the apparent oxygen utilization (AOU). The remaining of 75% was attributable to POC decomposition. However, the AOU contributable to DOC showed a function of latitude, with 15-55% found in the central subtropical Atlantic gyres and 15-25% in the equatorial region. The most likely explanation for the variation of DOC relative to POC degradation with respect to AOU was the regional variability in the export of POC, which was suggested to be highest in the high nutrient regions of the equator and at the poleward margins of the subtropical gyres. As a result, DOC formed an important contribution to AOU in oligotrophic regions, while POC was the dominant control of AOU in upwelling regions. Some freshly-produced fractions of DON and DOP with turnover times of months to years were capable of escaping rapid microbial degradation in surface waters and became entrained into deep waters via diffusive mixing. Subsequent microbial degradation of these DON and DOP took place in the thermocline, regenerating inorganic nutrients. Statistically significant correlations were observed between the DON-to-DIN and DOP-to-DIP relationships. Calculations of the fluxes of dissolved organic nutrients relative to inorganic nutrients suggested that in the upper thermocline (i.e. above 300 m), the downward fluxes of DON and DOP contributed to a total of 4% and 5% of the upward fluxes of DIN and DIP, respectively, into the euphotic zone. The remaining of 95% of the upward dissolved inorganic nutrients fell out of the euphotic zone as particles in order to prevent nutrient accumulation and to maintain nutrient integrity of the pelagic ecosystem.
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Kiker, Taylor Wilson. "Dissolved Organic Carbon and Dissolved Inorganic Carbon along an Urbanization Gradient in Charlotte, North Carolina." Thesis, The University of North Carolina at Charlotte, 2018. http://pqdtopen.proquest.com/#viewpdf?dispub=10928077.

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Streams and rivers are an integral component of the freshwater carbon cycle as they provide the lateral transport of carbon from terrestrial environments to the ocean. Urbanization is one of the fastest growing land uses and it has major impacts on streams and rivers. This study examined twenty-eight watersheds varying in land uses from pre-restoration forested to urban in Charlotte, North Carolina. Their impervious cover ranged from 0.5–55%. The objective of this study was to examine alterations to freshwater carbon processes among watersheds of various land uses in multiple streams in Mecklenburg County, Charlotte, NC.

Surface water was collected at each site in addition to discharge measurements. Water quality parameters were analyzed including: DOC concentration, Specific UV Absorbance of DOC, DIC concentration, alkalinity concentration, δ 13C-DIC, major cations (Na+, K+, Mg 2+, and Ca2+), and anions (F–, Cl–, PO43–, NO 3–and SO42–). DOC concentration ranged from 1.1–18 mg/L and SUVA values ranged from 0.2–18 L/mg*m. Alkalinity concentrations ranged from 0.1–3.8 meq/L and DIC concentrations ranged from 0.2–3.8 mM. δ13C-DIC values ranged from –18.0‰ to –7.4‰. Overall, DOC concentrations and SUVA values had weak negative relationships with percent impervious cover. DIC concentrations, alkalinity concentrations, δ13C-DIC values, all cations, and F–, Cl– , and SO42– had strong positive relationships with percent impervious cover. PO43– and NO 3– had weak correlations with percent impervious cover. The increase in DIC, alkalinity, δ13C-DIC, and cations with high impervious cover was largely due to the increased chemical weathering of concrete materials in urban areas.

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Gennings, Chad. "Photochemical oxidation of dissolved organic carbon in streams." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1999. http://www.collectionscanada.ca/obj/s4/f2/dsk2/ftp03/MQ39192.pdf.

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Chaichana, Saisiri. "Dissolved organic carbon and nitrogen in coastal waters." Thesis, University of East Anglia, 2017. https://ueaeprints.uea.ac.uk/62312/.

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Dissolved organic matter (DOM) including carbon and nitrogen (DOC and DON) are important but poorly understood components of the marine biogeochemical cycle. In this study, the distribution and cycling of DOC and DON, and particulate organic carbon and nitrogen (POC and PON) were investigated in North Sea surface and bottom water during the stratified summer season in 2011 and 2012, along with other key biogeochemical parameters such as nutrients. The summer DOC, DON, POC and PON ranged from 32.7-134.5, 2.8-13.7, 1.1-43.8 and 0.3-5.9 μM, respectively. The well-mixed water of the southern North Sea was also surveyed in the winter of 2011; measured concentration of DOC and DON were 56.2-224.8 and 3.7-12.3 μM. In summer, DOM and POM generally exhibited high levels in the southern well-mixed water (SM), whereas inorganic nutrient concentrations were higher in the northern bottom water (NB) due to nutrient regeneration and offshore water inflow. DOM in summer and inorganic nutrients in winter were also clearly influenced by riverine inputs. DON was the dominant nitrogen fraction of northern surface water and SM in summer, while in NB, TOxN (nitrate + nitrite) was the dominant fraction. Analysis of SmartBuoy samples show phytoplankton provided a net source of DOM over the spring bloom period with net degradation in autumn and winter. Incubation experiments on water collected from two North Sea sites in autumn, winter 2013 and spring 2014 showed no nutrient (N and P) limitation on DOM degradation. The experiments yield mean bacterial decay rate constants (for three seasons) at the two sites of 4 ± 8 and 2 ± 3 %d-1 kDOC and 3 ± 4 and 4 ± 4 %d-1 kDON, under dark conditions. In comparison to the Redfield ratio, the bulk C:N molar ratio is enriched in carbon relative to nitrogen, while the slope C:N ratio is close to the Redfield ratio, but with a background of high C:N material.
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Heyes, Andrew. "Mineral weathering by dissolved organic carbon in subarctic fens." Thesis, McGill University, 1990. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=59647.

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The contribution of dissolved organic carbon (DOC) to mineral weathering was investigated under the changing Eh and pH conditions in three subarctic fens, near Schefferville, Quebec. No evidence of increased weathering rates nor different weathering patterns were found in the fen basal sediment despite DOC-rich and low Eh (0 to +200 mV) conditions.
Solutions containing 50 mg DOC/L derived from subarctic fen peat, and of 50 and 300 mg DOC/L, derived from deciduous leaf litter were used as weathering agents. Clinochlore, microcline and the Fe-rich basal till from the Schefferville fens were used as weatherable mediums. The DOC rich solutions and controls (made of distilled water buffered to the same initial pH) were used to investigate the relative weathering ability of DOC-rich waters under aerobic and anaerobic conditions. The relative ability was determined by comparing the changing cation concentrations in the solutions.
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Hargette, Paul Hudson. "Removal of dissolved organic carbon and organic halide precursors by enhanced coagulation." Thesis, This resource online, 1997. http://scholar.lib.vt.edu/theses/available/etd-08252008-162839/.

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Murphy, Ellyn Margaret. "Carbon-14 measurements and characterization of dissolved organic carbon in ground water." Diss., The University of Arizona, 1987. http://hdl.handle.net/10150/191131.

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Carbon-14 was measured in the dissolved organic carbon (DOC) in ground water and compared with ¹⁴C analyses of dissolved inorganic carbon (DIC). Two field sites were used for this study; the Stripa mine in central Sweden, and the Milk River Aquifer in southern Alberta, Canada. The Stripa mine consists of a Precambrian granite dominated by fracture flow, while the Milk River Aquifer is a Cretaceous sandstone aquifer characterized by porous flow. At both field sites, ¹⁴C analyses of the DOC provide additional information on the ground-water age. At the Stripa site the DIC from the recharge area probably precipitates at around the 300 m level of the mine, never reaching the deeper ground waters. In this case, ¹⁴C analyses of the DOC provides a better estimate of the ground-water age. The dilution of the DIC by carbonates and microbial processes in the Milk River Aquifer is so great that geochemical corrections of ¹⁴C data are difficult. This is another example where ¹⁴C analyses of the DOC provide more information on ground-water age. Carbon-14 was measured on both the hydrophobic and hydrophilic organic fractions of the DOC. At the Stripa site, the hydrophobic organic compounds in the V2 borehole ranged from 7,500 to 15,500 years before present, suggesting a young component of ground water. Other hydraulic and isotopic evidence supports relatively recent ground water mixing with older brines in this borehole. The δ¹³C values of the DIC in the V2 borehole are light and similar to the stable carbon isotope values for the DOC, supporting a biogenic origin of the DIC. The organic compounds in the hydrophobic and hydrophilic fractions were also characterized. The DOC may originate from kerogen in the aquifer matrix, from soil organic matter in the recharge zone, or from a combination of these two sources. Carbon-14 analyses, along with characterization of the organics, were used to determine this origin. Carbon-14 analyses of the hydrophobic fraction in the Milk River Aquifer suggest a soil origin, while ¹⁴C analyses of the hydrophilic fraction suggest an origin within the Cretaceous sediments (kerogen) or from the shale in contact with the aquifer.
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McDonald, Adrian. "Fluorescence of dissolved organic matter in natural waters." Thesis, University of Southampton, 1998. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.243162.

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Johannessen, Sophia. "A photochemical sink for dissolved organic carbon in the ocean." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 2000. http://www.collectionscanada.ca/obj/s4/f2/dsk2/ftp02/NQ57364.pdf.

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Books on the topic "Dissolved organic carbon"

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Cussion, Sylvia. Dissolved organic carbon and total organic carbon in reagent water and effluent: Report. [Toronto]: Quality Management Office, Laboratory Services Branch, Ontario Ministry of the Environment, 1992.

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Knocke, William R. Impacts of dissolved organic carbon on iron removal. Denver, CO: The Foundation and American Water Works Association, 1993.

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LaZerte, Bruce. Metal transport and retention: The role of dissolved organic carbon. [Toronto]: Queen's Printer for Ontario, 1991.

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Lazerte, Bruce D. Metal transport and retention: The role of dissolved organic carbon. Toronto, Ont: Ministry of the Environment, 1991.

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Reilly, Timothy J. Dissolved pesticides, dissolved organic carbon, and water-quality characteristics in selected Idaho streams, April-December 2010. Reston, Va: U.S. Dept. of the Interior, U.S. Geological Survey, 2012.

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Sturman, Paul John. Control of acid rock drainage from mine tailings through the addition of dissolved organic carbon. Bozeman, MT: Montana State University, 2004.

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Salley, Betty A. Comparison study of five instruments measuring dissolved organic carbon for the Chespeake [sic] Bay Monitoring Program. Gloucester Point, Va: Virginia Institute of Marine Science, School of Marine Science, College of William and Mary, 1995.

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McCall, Jackie Kendal. Relationships among yellow substance, dissolved organic carbon, pH, and transparency in acidic lakes near Sudbury, Ontario. Sudbury, Ont: Laurentian University, Department of Geography, 1994.

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Beauclerc, Kaela B. The influence of dissolved organic carbon on the absorbance of ultraviolet light in Northern Ontario lakes. Sudbury, Ont: Laurentian University, Department of Biology, 2000.

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Goldstone, Jared Verrill. Direct and indirect photoreactions of chromophoric dissolved organic matter: Roles of reactive oxygen species and iron. Cambridge, Mass: Massachusetts Institute of Technology, 2002.

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Book chapters on the topic "Dissolved organic carbon"

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Thurman, E. M. "Classification of Dissolved Organic Carbon." In Organic Geochemistry of Natural Waters, 103–10. Dordrecht: Springer Netherlands, 1985. http://dx.doi.org/10.1007/978-94-009-5095-5_5.

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Thurman, E. M. "Functional Groups of Dissolved Organic Carbon." In Organic Geochemistry of Natural Waters, 87–101. Dordrecht: Springer Netherlands, 1985. http://dx.doi.org/10.1007/978-94-009-5095-5_4.

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Thurman, E. M. "Transport, Origin and Source of Dissolved Organic Carbon." In Organic Geochemistry of Natural Waters, 67–85. Dordrecht: Springer Netherlands, 1985. http://dx.doi.org/10.1007/978-94-009-5095-5_3.

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Suzuki, Yoshimi. "Dynamic Cycle of Dissolved Organic Carbon and Marine Productivity." In The Global Carbon Cycle, 531–49. Berlin, Heidelberg: Springer Berlin Heidelberg, 1993. http://dx.doi.org/10.1007/978-3-642-84608-3_21.

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Pignatello, Joseph J. "Adsorption of Dissolved Organic Compounds by Black Carbon." In Molecular Environmental Soil Science, 359–85. Dordrecht: Springer Netherlands, 2012. http://dx.doi.org/10.1007/978-94-007-4177-5_12.

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Long, Austin, Ellyn M. Murphy, Stanley N. Davis, and Robert M. Kalin. "Natural Radiocarbon in Dissolved Organic Carbon in Groundwater." In Radiocarbon After Four Decades, 288–308. New York, NY: Springer New York, 1992. http://dx.doi.org/10.1007/978-1-4757-4249-7_20.

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Caron, Gail, and I. H. Suffet. "Binding of Nonpolar Pollutants to Dissolved Organic Carbon." In Advances in Chemistry, 117–30. Washington, DC: American Chemical Society, 1988. http://dx.doi.org/10.1021/ba-1988-0219.ch009.

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Winterdahl, Mattias, Kevin Bishop, and Martin Erlandsson. "Acidification, Dissolved Organic Carbon (DOC) and Climate Change." In Global Environmental Change, 281–87. Dordrecht: Springer Netherlands, 2014. http://dx.doi.org/10.1007/978-94-007-5784-4_107.

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Prokushkin, A. S., S. Hobara, and S. G. Prokushkin. "Behavior of Dissolved Organic Carbon in Larch Ecosystems." In Ecological Studies, 205–28. Dordrecht: Springer Netherlands, 2009. http://dx.doi.org/10.1007/978-1-4020-9693-8_11.

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Moore, Tim R. "Dissolved Organic Carbon Production and Transport in Canadian Peatlands." In Carbon Cycling in Northern Peatlands, 229–36. Washington, D. C.: American Geophysical Union, 2013. http://dx.doi.org/10.1029/2008gm000816.

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Conference papers on the topic "Dissolved organic carbon"

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Zhao, Haiping, Qingxue Li, Xiaopeng Yue, and Jianhua Tao. "Ecohydrodynamic Modelling of Dissolved Organic Carbon Cycle." In 2009 3rd International Conference on Bioinformatics and Biomedical Engineering (iCBBE). IEEE, 2009. http://dx.doi.org/10.1109/icbbe.2009.5162674.

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Pipe-Martin, C. "Dissolved organic carbon removal by biological treatment." In WATER POLLUTION 2008. Southampton, UK: WIT Press, 2008. http://dx.doi.org/10.2495/wp080431.

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Wheatley, Rachel M., Siddhartha Mitra, Peter J. van Hengstum, Timothy Dellapenna, and D. Reide Corbett. "QUANTIFYING EXCHANGEABLE DISSOLVED ORGANIC CARBON DEPOSITED BY HURRICANE RAINWATER." In 68th Annual GSA Southeastern Section Meeting - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019se-327230.

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Yanhong, Xu, He Yuxin, Sun Yongge, and Pang Jiali. "The Contribution from Particulate Organic Carbon (Poc) to Dissolved Organic Carbon (Doc) in Eutrophic Lake Taihu, China." In 29th International Meeting on Organic Geochemistry. European Association of Geoscientists & Engineers, 2019. http://dx.doi.org/10.3997/2214-4609.201902927.

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Codden, Christina Jean, Catherine Edwards, Thais Bittar, Sasha Wagner, Robert Spencer, Sarah Ellen Johnston, and Aron Stubbins. "TEMPORALLY RESOLVED DISSOLVED ORGANIC CARBON DYNAMICS IN A GEORGIA SALTMARSH." In 53rd Annual GSA Northeastern Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018ne-310681.

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Yang, Ziming, Yiju Liao, and Alexandria Aspin. "Dissolved metal-mediated organic carbon transformations in oceanic hydrothermal systems." In Goldschmidt2022. France: European Association of Geochemistry, 2022. http://dx.doi.org/10.46427/gold2022.9958.

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Balogun, Fatai, Miranda Aiken, Alireza Namayandeh, Owen Duckworth, and Matthew Polizzotto. "DISSOLVED ORGANIC CARBON DIMINISHES MANGANESE OXIDE-DRIVEN OXIDATION OF CHROMIUM." In GSA Connects 2021 in Portland, Oregon. Geological Society of America, 2021. http://dx.doi.org/10.1130/abs/2021am-367257.

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Pipko, Irina, and Svetlana Pugach. "Dynamics of dissolved carbon and optical characteristics of dissolved organic matter in the Siberian rivers." In 28th International Symposium on Atmospheric and Ocean Optics: Atmospheric Physics, edited by Oleg A. Romanovskii and Gennadii G. Matvienko. SPIE, 2022. http://dx.doi.org/10.1117/12.2644879.

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Goodwin, Janae, Iliomar Rodriguez-Ramos, Breanna H. Taylor, Alondra Mercado-mercado, Mouhamadou Kane, Isabella B. Bennett, Julia Perdrial, and Paul R. Bierman. "EVALUATING E. COLI, DISSOLVED ORGANIC CARBON, AND TOTAL DISSOLVED NITROGEN WITHIN TWO SOUTHEASTERN PUERTO RICO WATERSHEDS." In GSA Connects 2022 meeting in Denver, Colorado. Geological Society of America, 2022. http://dx.doi.org/10.1130/abs/2022am-382818.

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Qiong, Liu, Delu Pan, Haiqing Huang, Jianxin Lu, and Qiankun Zhu. "Relationship between the colored dissolved organic matter and dissolved organic carbon and the application on remote sensing in East China Sea." In SPIE Remote Sensing. SPIE, 2011. http://dx.doi.org/10.1117/12.897865.

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Reports on the topic "Dissolved organic carbon"

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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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Daniel J. Repeta. Seqestration of dissolved organic carbon in the deep sea. Office of Scientific and Technical Information (OSTI), March 2006. http://dx.doi.org/10.2172/908226.

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Thomas, James, David Decker, Gary Patterson, Zell Peterman, Todd Mihevc, Jessica Larsen, and Ronald Hershey. Yucca Mountain Area Saturated Zone Dissolved Organic Carbon Isotopic Data. Office of Scientific and Technical Information (OSTI), June 2007. http://dx.doi.org/10.2172/909181.

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Miller, William L. Relating Ocean Optics to Photochemical Transformations of Dissolved Organic Carbon. Fort Belvoir, VA: Defense Technical Information Center, September 2002. http://dx.doi.org/10.21236/ada629182.

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KAPLAN, DANIEL. Influence of Dissolved Organic Carbon and pH on Containment Sorption to Sediment. Office of Scientific and Technical Information (OSTI), September 2004. http://dx.doi.org/10.2172/835584.

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Chipman, D. W., and T. Takahashi. Development of gas chromatographic system for dissolved organic carbon analysis in seawater. Office of Scientific and Technical Information (OSTI), December 1992. http://dx.doi.org/10.2172/6834139.

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Benner, R. Mechanisms of dissolved organic carbon cycling in an ocean margin. Final technical report. Office of Scientific and Technical Information (OSTI), November 1997. http://dx.doi.org/10.2172/584909.

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Miller, William L. Relating Ocean Optics to Photochemical Transformations of Dissolved Organic Carbon in Coastal Waters. Fort Belvoir, VA: Defense Technical Information Center, September 2001. http://dx.doi.org/10.21236/ada622160.

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Hershey, Ronald L., Wyall Fereday, and James M. Thomas. Dissolved Organic Carbon 14C in Southern Nevada Groundwater and Implications for Groundwater Travel Times. Office of Scientific and Technical Information (OSTI), August 2016. http://dx.doi.org/10.2172/1287225.

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