Academic literature on the topic 'Stabilization of soil organic matter'

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Journal articles on the topic "Stabilization of soil organic matter"

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Biryukov, M. V., I. M. Ryzhova, A. A. Gunina, L. G. Bogatyrev, and E. A. Pogozheva. "Stabilization of organic matter in soil lysimeters." Moscow University Soil Science Bulletin 69, no. 2 (April 2014): 55–61. http://dx.doi.org/10.3103/s0147687414020021.

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Rennert, T., and H. Pfanz. "Geogenic CO2affects stabilization of soil organic matter." European Journal of Soil Science 66, no. 5 (July 14, 2015): 838–46. http://dx.doi.org/10.1111/ejss.12284.

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Mueller, Carsten W., Carmen Hoeschen, Markus Steffens, Henning Buddenbaum, Kenneth Hinkel, James G. Bockheim, and Jenny Kao-Kniffin. "Microscale soil structures foster organic matter stabilization in permafrost soils." Geoderma 293 (May 2017): 44–53. http://dx.doi.org/10.1016/j.geoderma.2017.01.028.

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Adamczyk, Bartosz. "How do terrestrial plants access high molecular mass organic nitrogen, and why does it matter for soil organic matter stabilization?" Plant and Soil 465, no. 1-2 (June 10, 2021): 583–92. http://dx.doi.org/10.1007/s11104-021-05022-8.

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AbstractAlthough there is increasing awareness of the potential role of organic N compounds (ON) in plant nutrition, its implications for soil organic matter (SOM) stabilization have hardly been discussed yet. The aim of this paper is therefore to gather the newest insights into plant use of high molecular mass organic N, its effect on root growth and anatomy, and finally, to discuss the implications of plant use of organic N for SOM stabilization. I propose that modified root growth due to the uptake of ON provides greater root and root-associated microbe input, leading to enhanced SOM stabilization. Finally, I discuss the role of the proposed framework in different ecosystems, and I encourage future studies combining plant N nutrition and SOM stabilization.
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Spielvogel, S., J. Prietzel, and I. Kgel-Knabner. "Soil organic matter stabilization in acidic forest soils is preferential and soil type-specific." European Journal of Soil Science 59, no. 4 (August 2008): 674–92. http://dx.doi.org/10.1111/j.1365-2389.2008.01030.x.

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Polyakov, Vyacheslav, and Evgeny Abakumov. "Assessments of Organic Carbon Stabilization Using the Spectroscopic Characteristics of Humic Acids Separated from Soils of the Lena River Delta." Separations 8, no. 6 (June 20, 2021): 87. http://dx.doi.org/10.3390/separations8060087.

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In the Arctic zone, where up to 1024 × 1013 kg of organic matter is stored in permafrost-affected soils, soil organic matter consists of about 50% humic substances. Based on the analysis of the molecular composition of humic acids, we assessed the processes of accumulation of the key structural fragments, their transformations and the stabilization rates of carbon pools in soils in general. The landscape of the Lena River delta is the largest storage of stabilized organic matter in the Arctic. There is active accumulation and deposition of a significant amount of soil organic carbon from terrestrial ecosystems in a permafrost state. Under ongoing climate change, carbon emission fluxes into the atmosphere are estimated to be higher than the sequestration and storing of carbon compounds. Thus, investigation of soil organic matter stabilization mechanisms and rates is quite an urgent topic regarding polar soils. For study of molecular elemental composition, humic acids were separated from the soils of the Lena River delta. Key structural fragments of humic matter were identified and quantified by CP/MAS 13C NMR spectroscopy: carboxyl (–COOR); carbonyl (–C=O); CH3–; CH2–; CH-aliphatic; –C-OR alcohols, esters and carbohydrates; and the phenolic (Ar-OH), quinone (Ar = O) and aromatic (Ar–) groups as benchmark Cryosols of the Lena delta river terrestrial ecosystem. Under the conditions of thermodynamic evolutionary selection, during the change between the dry and wet seasons, up to 41% of aromatic and carboxyl fragments accumulated in humic acids. Data obtained showed that three main groups of carbon played the most important role in soil organic matter stabilization, namely C, H-alkyls ((CH2)n/CH/C and CH3), aromatic compounds (C-C/C-H, C-O) and an OCH group (OCH/OCq). The variations of these carbon species’ content in separated humics, with special reference to soil–permafrost organic profiles’ recalcitrance in the current environment, is discussed.
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Eusterhues, Karin, Cornelia Rumpel, and Ingrid Kögel-Knabner. "Stabilization of soil organic matter isolated via oxidative degradation." Organic Geochemistry 36, no. 11 (November 2005): 1567–75. http://dx.doi.org/10.1016/j.orggeochem.2005.06.010.

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Ling, Felix Ngee Leh, Khairul Anuar Kassim, Ahmad Tarmizi Abdul Karim, and Tze Wei Chan. "Stabilization of Artificial Organic Soil at Room Temperature Using Blended Lime Zeolite." Advanced Materials Research 723 (August 2013): 985–92. http://dx.doi.org/10.4028/www.scientific.net/amr.723.985.

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Organic content in soil is believed to inhibit formation of reaction products in lime stabilization which resulted in low gain of strength when dealing with organic soils. Zeolite, a kind of pozzolan with high CEC capacity is proposed to be use in this study in order to improve lime stabilization of organic soil. The effectiveness of blended lime zeolite in stabilization of organic soils was investigated by using two types of artificial organic soils with predetermined organic contents. Artificial organic soils were formed by mixing inorganic soil (commercial kaolin) with organic matter (commercial humic acid) at specific ratio. Initial consumption of lime for organic soils was determined in order to determine the minimum percentage of stabilizer required for each soil. Potential influencing factors that might affect the strength such as organic contents, contents of stabilizer, and curing periods were studied. The findings of the study showed that high organic contents and low lime contents resulted in lower gain of strength. However, it is found that slight replacement of lime with zeolite works well with low organic soil at long curing period which resulted in highest strength among all the mixes. Overall, longer curing periods will increase the strength of the soil in the order of 56 days > 28 days > 7 days. Nevertheless, the percentage of strength increment over curing periods is linear with the lime contents, which proved that lime is required for pozzolanic reaction.
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Basler, A., M. Dippold, M. Helfrich, and J. Dyckmans. "Microbial carbon recycling: an underestimated process controlling soil carbon dynamics – Part 2: A C<sub>3</sub>-C<sub>4</sub> vegetation change field labelling experiment." Biogeosciences 12, no. 21 (November 5, 2015): 6291–99. http://dx.doi.org/10.5194/bg-12-6291-2015.

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Abstract. The mean residence times (MRT) of different compound classes of soil organic matter (SOM) do not match their inherent recalcitrance to decomposition. One reason for this is the stabilization within the soil matrix, but recycling, i.e. the reuse of "old" organic material to form new biomass may also play a role as it uncouples the residence times of organic matter from the lifetime of discrete molecules in soil. We analysed soil sugar dynamics in a natural 30-year old labelling experiment after a wheat-maize vegetation change to determine the extent of recycling and stabilization by assessing differences in turnover dynamics between plant and microbial-derived sugars: while plant-derived sugars are only affected by stabilization processes, microbial sugars may be subject to both, stabilization and recycling. To disentangle the dynamics of soil sugars, we separated different density fractions (free particulate organic matter (fPOM), light occluded particulate organic matter (≤ 1.6 g cm−3; oPOM1.6), dense occluded particulate organic matter (≤ 2 g cm−3; oPOM2) and mineral-associated organic matter (> 2 g cm−3; mineral)) of a silty loam under long-term wheat and maize cultivation. The isotopic signature of neutral sugars was measured by high pressure liquid chromatography coupled to isotope ratio mass spectrometry (HPLC/IRMS), after hydrolysis with 4 M Trifluoroacetic acid. While apparent MRT of sugars were comparable to total organic carbon in the bulk soil and mineral fraction, the apparent MRT of sugar carbon in the oPOM fractions were considerably lower than those of the total carbon of these fractions. This indicates that oPOM formation was fuelled by microbial activity feeding on new plant input. In the bulk soil, MRT of the mainly plant-derived xylose were significantly lower than those of mainly microbial-derived sugars like galactose, rhamnose, fucose, indicating that recycling of organic matter is an important factor regulating organic matter dynamics in soil.
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Tremblay, Hélène, Josée Duchesne, Jacques Locat, and Serge Leroueil. "Influence of the nature of organic compounds on fine soil stabilization with cement." Canadian Geotechnical Journal 39, no. 3 (June 1, 2002): 535–46. http://dx.doi.org/10.1139/t02-002.

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It is well known that organic matter may affect the cementing process in soils, but what happens when cement is added to an organic soil? Both the organic matter content and the nature of this organic matter affect the properties of a treated soil. It appears that some organic compounds delay or even inhibit the hydration process of cement, while others do not affect the reaction at all. This paper presents some results of a laboratory study in which 13 different organic compounds were added separately to two different soils, and then treated with 10% cement. To assess the cementing process, undrained shear strength was measured on the different specimens, and some chemical analyses were performed on the pore liquid. The results indicate that the organic acids producing a pH lower than 9 in the pore solution strongly affect the development of cementing products and almost no strength gain was noted. Also, oils and hydrocarbons, which are insoluble in water, delay the cement hydration but do not affect the final strength. Finally, the pH value and the SO4 concentration in the pore solution are good indicators of the cementing effectiveness of the treated specimens.Key words: soil stabilization, organic compounds, undrained shear strength, cement, chemical analyses.
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Dissertations / Theses on the topic "Stabilization of soil organic matter"

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Doohan, Thomas James. "Drivers of Soil Organic Matter Stabilization across Ohio." The Ohio State University, 2020. http://rave.ohiolink.edu/etdc/view?acc_num=osu1597941993038872.

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Poirier, Vincent. "Investigating the mechanisms of soil organic matter stabilization in a clayey soil of the St-Lawrence lowlands, Québec, Canada." Thesis, McGill University, 2011. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=104764.

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Soil organic matter (SOM) is a key element in soil quality and productivity, and represents the biggest C pool of the terrestrial biosphere. Understanding soil organic carbon (SOC) retention mechanisms is necessary to address their role as potential C sink, and ensure their quality and productivity for future generations. The objective of this research was to examine, under controlled conditions, the stabilization of newly added C and N coming from crop residues in topsoil and subsoil horizons of a heavy clay soil from the St-Lawrence Lowlands. Topsoil (0-20 cm depth, 31.3 g SOC kg-1 soil) and subsoil (30-70 cm depth, 4.5 g SOC kg-1 soil) were incubated (25ºC, -38 kPa, C/N = 10) for 51 d with increasing amounts (from 0 to 40 g C kg-1 soil) of 13C-15N-labelled corn residues. Carbon mineralization was greater in topsoil than subsoil, but comparable amounts of residue-C were retained in both soils, on a whole soil basis. This suggests that the extra C lost from the topsoil came from the mineralization of autochthonous SOC. Preferential retention of residue-derived C and N occurred in large macroaggregates (>1000 µm) in the subsoil, and in small macroaggregates (250-1000 µm) in the topsoil. Macroaggregate enrichment in residue-derived C and N occurred simultaneously through small-scale adsorption (< 50 µm) and large-scale occlusion (>250 µm). Sequential density fractionation of soil coupled with X-ray diffraction mineralogical analysis revealed a greater proportion of autochthonous and residue-derived C and N associated with soil minerals in subsoil than topsoil. Subsoil organo-mineral complexes were enriched in residue-derived N, indicating preferential adsorption of nitrogenous compounds onto unsaturated mineral surfaces in the early stages of organo-mineral complexes formation. In conclusion, topsoil and subsoil horizons of a heavy clay soil from Eastern Canada can accumulate substantial amounts of residue-derived C and N, with greater potential for C and N sequestration in stable organo-mineral complexes in subsoil than topsoil.
La matière organique du sol (MOS) assure la qualité et la productivité du sol et représente le plus grand réservoir de C de la biosphère terrestre. Comprendre les mécanismes de rétention du carbone organique du sol (COS) s'avère essentiel pour évaluer le potentiel des sols à agir comme puits de C et pour assurer leur qualité et leur productivité futures. La présente recherche visait à évaluer, en conditions contrôlées, la stabilisation du C et de l'N provenant de résidus de culture nouvellement incorporés dans les horizons superficiel et profond d'un sol argileux des Basses-Terres du St-Laurent. Des échantillons de sol des horizons superficiel (0-20 cm, 31.3 g COS kg-1 sol) et profond (30-70 cm, 4.5 g COS kg-1 sol) ont été incubés (25ºC, -38 kPa, C/N=10) pendant 51 jours avec des doses croissantes (0 à 40 g C kg-1 sol) de résidus de maïs enrichis en 13C et 15N. La minéralisation du C était plus importante dans l'horizon superficiel que dans l'horizon profond, alors que la quantité de nouveau C retenue dans le sol entier était similaire dans les deux horizons, suggérant ainsi qu'une minéralisation du COS autochtone est survenue. Le C et l'N des résidus ont été retenus préférentiellement dans les grands macroagrégats (>1000 µm) dans l'horizon profond, mais dans les petits macroagrégats (250-1000 µm) dans l'horizon superficiel. L'enrichissement des macroagrégats en C et N nouveaux s'est produit par adsorption à petite échelle (< 50 µm) et par occlusion à grande échelle (>250 µm) simultanément dans le sol. Le fractionnement densimétrique couplé à l'analyse minéralogique du sol a révélé qu'une proportion plus grande du C et de l'N autochtones et provenant des résidus était associée aux phases minérales dans l'horizon profond que dans l'horizon superficiel. Les complexes organo-minéraux de l'horizon profond étaient enrichis en N autochtone et provenant des résidus, ce qui indique une adsorption préférentielle des composés azotés sur les surfaces minérales non saturées lors des premières étapes de formation des complexes organo-minéraux. Ainsi, les horizons superficiel et profond étudiés peuvent tous deux accumuler davantage de C et d'N provenant des résidus, mais le potentiel de séquestration du C et de l'N par association organo-minérale stable s'avère plus important dans l'horizon profond que dans l'horizon superficiel.
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Andruschkewitsch, Rouven [Verfasser]. "Effects of different tillage treatments on labile soil organic matter pools and stabilization processes / Rouven Andruschkewitsch." Kassel : Universitätsbibliothek Kassel, 2013. http://d-nb.info/103872354X/34.

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Mikutta, Robert. "Stabilization of organic matter in the acid soil environment : importance of mineral phases and involved mechanisms /." Tönning ; Lübeck Marburg : Der Andere Verl, 2007. http://bvbr.bib-bvb.de:8991/F?func=service&doc_library=BVB01&doc_number=016441507&line_number=0001&func_code=DB_RECORDS&service_type=MEDIA.

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Ndossi, Emanueli Mathayo [Verfasser]. "Composition, degradation and stabilization of soil organic matter along an elevation gradient of Mount Kilimanjaro / Emanueli Mathayo Ndossi." Göttingen : Niedersächsische Staats- und Universitätsbibliothek Göttingen, 2020. http://d-nb.info/122410031X/34.

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Schmidt, Jana [Verfasser], Beate [Gutachter] Michalzik, and Francois [Gutachter] Buscot. "Stabilization and dynamics of soil organic matter in response to long-term mineral and organic fertilization / Jana Schmidt ; Gutachter: Beate Michalzik, Francois Buscot." Jena : Friedrich-Schiller-Universität Jena, 2018. http://d-nb.info/1205884424/34.

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Vázquez-Ortega, Angélica. "Coupled Transport, Fractionation and Stabilization of Dissolved Organic Matter and Rare Earth Elements in the Critical Zone." Diss., The University of Arizona, 2013. http://hdl.handle.net/10150/301696.

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It is important to understand the processes that influence the critical zone (CZ) evolution to ensure its sustainability. This thesis reports on laboratory and field experiments designed to measure the behavior of biogenic and lithogenic chemical species and their interaction in the CZ from column to pedon to catchment scales. We postulated that interactions between organic matter and rock-derived metals drive coupled processes of carbon stabilization and chemical weathering and denudation in the Jemez River Basin Critical Zone Observatory (JRB-CZO). First, we observed that secondary mineral coatings (Al and Fe (oxy)hydroxides) on primary silicate surfaces play a major role in sequestering aromatic and "humified" dissolved organic matter (DOM) into sorbate form, significantly retarding their subsurface transport. Further, reinfusion to OM-reacted-porous-media of a different DOM source resulted in exchange reactions consistent with a zonal model of OM adsorption at mineral surfaces. This dissertation also aimed to examine the influence of water and DOM fluxes on the CZ weathering processes. Rare earth elements (REE) were selected because of their coherent trends in reactivity toward organic ligands common to soils. Specifically, trends in REE fractionation were explored for their utility to inform on biogeochemical weathering processes in forested terrain in the JRB-CZO. Mineral weathering mechanisms are expected to differentially influence REE release, fractionation, and transport and the relative importance of such processes should be reflected in REE signatures of bulk soil, pore and surface waters. Our studies showed: (1) REE depletion trends with depth in bulk soils are correlated with topographically-induced variation in water and dissolved organic carbon (DOC) flux (reflected in negative correlations between total water and C fluxes) and solid phase REE concentrations measured at the same depths; (2) REE and DOC concentrations in stream waters were strongly correlated during snowmelt periods of high discharge, consistent with REE complexation and mobilization in association with organic ligands during shallow subsurface flow; (3) preferential sequestration of Eu occurs during formation of secondary Mn(IV)-oxides, explaining patterns of Eu enrichment in bulk soils; and (4) the incremental increase in positive Ce-anomalies with depth in bulk soils are apparently controlled by adsorption/co-precipitation with secondary Fe-(oxy)hydroxide minerals.
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Bimüller, Carolin Verfasser], Ingrid [Akademischer Betreuer] [Kögel-Knabner, and Heinz [Akademischer Betreuer] Flessa. "From leaf to soil - Nitrogen partitioning and stabilization in soil organic matter / Carolin Bimüller. Gutachter: Ingrid Kögel-Knabner ; Heinz Flessa. Betreuer: Ingrid Kögel-Knabner." München : Universitätsbibliothek der TU München, 2014. http://d-nb.info/1066985952/34.

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Graf-Rosenfellner, Markus [Verfasser], Martin [Akademischer Betreuer] Kaupenjohann, Martin [Gutachter] Kaupenjohann, and Friederike [Gutachter] Lang. "Soil organic matter in riparian floodplain soils : regionalization of stocks and stabilization processes / Markus Graf-Rosenfellner ; Gutachter: Martin Kaupenjohann, Friederike Lang ; Betreuer: Martin Kaupenjohann." Berlin : Technische Universität Berlin, 2016. http://d-nb.info/1156274958/34.

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Shahbaz, Muhammad Verfasser], Yakov [Akademischer Betreuer] [Kuzyakov, Andrea [Gutachter] Carminati, Felix [Gutachter] Heitkamp, and Evgenia [Gutachter] Blagodatskaya. "Crop residue decomposition and stabilization in soil organic matter / Muhammad Shahbaz ; Gutachter: Andrea Carminati, Felix Heitkamp, Evgenia Blagodatskaya ; Betreuer: Yakov Kuzyakov." Göttingen : Niedersächsische Staats- und Universitätsbibliothek Göttingen, 2017. http://d-nb.info/1125712996/34.

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Books on the topic "Stabilization of soil organic matter"

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Kumada, Kyōichi. Chemistry of soil organic matter. Tokyo: Japan Scientific Societies Press, 1987.

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Powlson, David S., Pete Smith, and Jo U. Smith, eds. Evaluation of Soil Organic Matter Models. Berlin, Heidelberg: Springer Berlin Heidelberg, 1996. http://dx.doi.org/10.1007/978-3-642-61094-3.

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Magdoff, F. R., M. A. Tabatabai, and E. A. Hanlon, eds. Soil Organic Matter: Analysis and Interpretation. Madison, WI, USA: Soil Science Society of America, 1996. http://dx.doi.org/10.2136/sssaspecpub46.

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Rees, R. M., B. C. Ball, C. D. Campbell, and C. A. Watson, eds. Sustainable management of soil organic matter. Wallingford: CABI, 2001. http://dx.doi.org/10.1079/9780851994659.0000.

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Vaughan, D., and R. E. Malcolm, eds. Soil Organic Matter and Biological Activity. Dordrecht: Springer Netherlands, 1985. http://dx.doi.org/10.1007/978-94-009-5105-1.

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Vityakon, Patma. Soil organic matter and soil quality in Northeast Thailand. Khon Kaen, Thailand: Department of Plant Science and Agricultural Resources, Faculty of Agriculture, Khon Kaen University, 2011.

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Soil organic matter: Biological and ecological effects. Malabar, Fla: Krieger, 1992.

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Tate, Robert L. Soil organic matter: Biological and ecological effects. New York: Wiley, 1987.

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Björklund, Pedro A. Soil organic matter: Ecology, environmental impact, and management. Hauppauge, N.Y: Nova Science Publishers, 2011.

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Campbell, C. A. Response of soil organic matter to crop management. Ottawa, Ont: Agriculture and Agri-Food Canada, Research Branch, 1996.

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Book chapters on the topic "Stabilization of soil organic matter"

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Rani, Sneha. "Clay Mineralogy: Soil Carbon Stabilization and Organic Matter Interaction." In Soil Carbon Stabilization to Mitigate Climate Change, 83–123. Singapore: Springer Singapore, 2021. http://dx.doi.org/10.1007/978-981-33-6765-4_3.

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Zhang, M., D. M. Fan, Q. Zhu, Y. P. Luo, and X. C. Wang. "Contribution of High Accumulated Polyphenols to C Stabilization in Soil of Tea Gardens." In Functions of Natural Organic Matter in Changing Environment, 397–400. Dordrecht: Springer Netherlands, 2012. http://dx.doi.org/10.1007/978-94-007-5634-2_72.

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González-Vila, F. J., G. Almendros, J. A. González-Pérez, Z. Hernández, H. Knicker, A. Piedra-Buena, and J. M. de la Rosa. "Structural Features of Humic Substances as Biogeochemical Proxies for Soil Carbon Stabilization and Ecosystem Functions." In Functions of Natural Organic Matter in Changing Environment, 391–95. Dordrecht: Springer Netherlands, 2012. http://dx.doi.org/10.1007/978-94-007-5634-2_71.

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Tatzber, Michael, Sabine Klepsch, Gerhard Soja, Thomas Reichenauer, Heide Spiegel, and Martin H. Gerzabek. "Determination of Soil Organic Matter Features of Extractable Fractions Using Capillary Electrophoresis: An Organic Matter Stabilization Study in a Carbon-14-Labeled Long-Term Field Experiment." In Labile Organic Matter-Chemical Compositions, Function, and Significance in Soil and the Environment, 23–40. Madison, WI, USA: Soil Science Society of America, Inc., 2015. http://dx.doi.org/10.2136/sssaspecpub62.2014.0033.

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Reddy, P. Parvatha. "Soil Organic Matter." In Sustainable Intensification of Crop Production, 157–73. Singapore: Springer Singapore, 2016. http://dx.doi.org/10.1007/978-981-10-2702-4_11.

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Powlson, David, Pete Smith, and Maria De Nobili. "Soil organic matter." In Soil Conditions and Plant Growth, 86–131. Oxford: Blackwell Publishing Ltd, 2013. http://dx.doi.org/10.1002/9781118337295.ch4.

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Blume, Hans-Peter, Gerhard W. Brümmer, Heiner Fleige, Rainer Horn, Ellen Kandeler, Ingrid Kögel-Knabner, Ruben Kretzschmar, Karl Stahr, and Berndt-Michael Wilke. "Soil Organic Matter." In Scheffer/SchachtschabelSoil Science, 55–86. Berlin, Heidelberg: Springer Berlin Heidelberg, 2015. http://dx.doi.org/10.1007/978-3-642-30942-7_3.

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Lal, R. "Soil: Organic Matter." In Landscape and Land Capacity, 267–71. Second edition. | Boca Raton: CRC Press, [2020] | Revised edition of: Encyclopedia of natural resources. [2014].: CRC Press, 2020. http://dx.doi.org/10.1201/9780429445552-35.

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Osman, Khan Towhid. "Soil Organic Matter." In Soils, 89–96. Dordrecht: Springer Netherlands, 2012. http://dx.doi.org/10.1007/978-94-007-5663-2_7.

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Merckx, Roel, Jan Diels, Bernard Vanlauwe, Nteranya Sanginga, Karolien Denef, and Koen Oorts. "Soil Organic Matter and Soil Fertility." In Sustaining Soil Fertility in West Africa, 69–89. Madison, WI, USA: Soil Science Society of America and American Society of Agronomy, 2015. http://dx.doi.org/10.2136/sssaspecpub58.ch4.

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Conference papers on the topic "Stabilization of soil organic matter"

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Abakumov, E., V. Polyakov, E. Pershina, and E. Ivanova. "Stabilization of soil organic matter and development microbial community in chronoseries of soils formation of south taiga ecosystem (bars of Ladoga Lake, Russian North-West)." In Fifth International Conference of CIS IHSS on Humic Innovative Technologies «Humic substances and living systems». CLUB PRINT ltd., 2019. http://dx.doi.org/10.36291/hit.2019.abakumov.068.

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Ouedraogo, F., L. Denaix, M. Sourzac, C. Coriou, S. Bussiere, S. Millin, N. Janot, J. Cornu, N. Fanin, and E. Parlanti. "DOES TEMPERATURE AFFECT SOIL ORGANIC MATTER DECOMPOSITION AND DISSOLVED ORGANIC MATTER OPTICAL PROPERTIES?" In 30th International Meeting on Organic Geochemistry (IMOG 2021). European Association of Geoscientists & Engineers, 2021. http://dx.doi.org/10.3997/2214-4609.202134202.

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B K Gelder and R P Anex. "Estimating Soil Organic Matter Using Aerial Imagery and Soil Surveys." In 2009 Reno, Nevada, June 21 - June 24, 2009. St. Joseph, MI: American Society of Agricultural and Biological Engineers, 2009. http://dx.doi.org/10.13031/2013.27306.

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Bartlova, Jaroslava. "INFLUENCE OF SOIL ORGANIC MATTER ON ITS WATER STABILITY OF SOIL AGGREGATES." In 17th International Multidisciplinary Scientific GeoConference SGEM2017. Stef92 Technology, 2017. http://dx.doi.org/10.5593/sgem2017/32/s13.043.

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Tallamy Glazer, Christine, Susan Crow, Hannah Hubanks, Francesca Cotrufo, and Michelle Haddix. "Mineral Associated Organic Matter and Soil Health in Hawaii." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.2540.

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Wang, Yinghui, Yameng Shi, Guodong Sun, Jintao Li, Huan Chen, Alex Chow, Hamed Majidzadeh, and Jun-Jian Wang. "Molecular-Level Soil Organic Matter Composition Under Impervious Surfaces." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.2791.

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Li, Runkui, Yasuyuki Kono, Junzhi Liu, Ming Peng, Venkatesh Raghavan, and Xianfeng Song. "Soil organic matter mapping with fuzzy logic and GIS." In IGARSS 2012 - 2012 IEEE International Geoscience and Remote Sensing Symposium. IEEE, 2012. http://dx.doi.org/10.1109/igarss.2012.6351375.

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Fasheng Zhang, Zuoxin Liu, Xiaoyuan Geng, and Zhenying Wang. "Mapping surface soil organic matter based on multispectral image." In 2010 International Conference on Image Analysis and Signal Processing. IEEE, 2010. http://dx.doi.org/10.1109/iasp.2010.5476123.

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Vizka, Elaine, Jonathan Deenik, Hannah Hubanks, and Susan Crow. "Climate-Wise Management: Soil Mineralogy’s Primary Influence on Soil Organic Matter in Hawaiʻi." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.2690.

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Jinliang, Wang, Qin Qiming, Dong Heng, Chen Chao, and Meng Qingye. "Study on Quantitative Retrieval of Soil Organic Matter Based on Bare Soil Spectrum." In 3rd International Conference on Multimedia Technology(ICMT-13). Paris, France: Atlantis Press, 2013. http://dx.doi.org/10.2991/icmt-13.2013.47.

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Reports on the topic "Stabilization of soil organic matter"

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Santschi, Peter H., Kathleen A. Schwehr, Chen Xu, Matthew Athon, Yi-Fang Ho, Patrick G. Hatcher, Nicole Didonato, and Daniel I. Kaplan. Plutonium Immobilization and Mobilization by Soil Organic Matter. Office of Scientific and Technical Information (OSTI), March 2016. http://dx.doi.org/10.2172/1240745.

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Wright, Alan L., and Edward A. Hanlon. Organic matter and soil structure in the Everglades Agricultural Area. Office of Scientific and Technical Information (OSTI), January 2013. http://dx.doi.org/10.2172/1337170.

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Dillon, Megan. A Study of Soil Organic Matter and Its Controlling Factors in Portland, Oregon. Portland State University Library, January 2000. http://dx.doi.org/10.15760/etd.155.

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Lesschen, Jan Peter, Theun Vellinga, Sanne Dekker, Annelotte van der Linden, and Rene Schils. Possibilities for monitoring CO2 sequestration and decomposition of soil organic matter on dairy farms. Wageningen: Wageningen Environmental Research, 2020. http://dx.doi.org/10.18174/526420.

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Knoepp, Jennifer D., Larry L. Tieszen, and Glen G. Fredlund. Assessing the vegetation history of three Southern Appalachian balds through soil organic matter analysis. Asheville, NC: U.S. Department of Agriculture, Forest Service, Southern Research Station, 1998. http://dx.doi.org/10.2737/srs-rp-013.

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Knoepp, Jennifer D., Larry L. Tieszen, and Glen G. Fredlund. Assessing the vegetation history of three Southern Appalachian balds through soil organic matter analysis. Asheville, NC: U.S. Department of Agriculture, Forest Service, Southern Research Station, 1998. http://dx.doi.org/10.2737/srs-rp-13.

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Jarvis, Stacey, Thomas Douglas, Karen Foley, Robert Jones, John Anderson, Stephen Newman, and Robyn Bartaro. Spectral assessment of soil properties : standoff quantification of soil organic matter content in surface mineral soils and Alaskan peat. Engineer Research and Development Center (U.S.), September 2017. http://dx.doi.org/10.21079/11681/22904.

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Amaranthus, Michael P., Debbie Page-Dumroese, Al Harvey, Efren Cazares, and Larry F. Bednar. Soil compaction and organic matter affect conifer seedling nonmycorrhizal and ectomycorrhizal root tip abundance and diversity. Portland, OR: U.S. Department of Agriculture, Forest Service, Pacific Northwest Research Station, 1996. http://dx.doi.org/10.2737/pnw-rp-494.

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DUDKINA, T. A. INCORPORATION OF ORGANIC MATTER INTO THE SOIL IN CROP ROTATIONS WITH DIFFERENT RATIOS OF CROP GROUPS. Ljournal, 2019. http://dx.doi.org/10.18411/issn1997-0749.2019-08-38-41.

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Devine, Warren D., and Constance A. Harrington. Effects of vegetation control and organic matter removal on soil water content in a young Douglas-fir plantation. Portland, OR: U.S. Department of Agriculture, Forest Service, Pacific Northwest Research Station, 2006. http://dx.doi.org/10.2737/pnw-rp-568.

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