Relevant bibliographies by topics / Soil horizons

Contents

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

Academic literature on the topic 'Soil horizons'

Author: Grafiati
Published: 4 June 2021
Last updated: 1 February 2022

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Journal articles on the topic "Soil horizons"

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Webb, T. H. "Identification of functional horizons to predict physical properties for soils from alluvium in Canterbury, New Zealand." Soil Research 41, no. 5 (2003): 1005. http://dx.doi.org/10.1071/sr01077.

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Lack of soil physical data, particularly soil water release data and hydraulic conductivity data, is recognised as one of the greatest limitations to the widespread application of simulation models, needed to address environmental issues. Because of the expense of generating new soil physical data pedotransfer functions may be used to predict soil physical data from existing information, notably soil morphology. Pedological horizon descriptions can then be used to estimate soil physical properties for many points in the landscape. The soils used in this study were derived from a systematic sam
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Herrmann, Dustin L., Laura A. Schifman, and William D. Shuster. "Widespread loss of intermediate soil horizons in urban landscapes." Proceedings of the National Academy of Sciences 115, no. 26 (2018): 6751–55. http://dx.doi.org/10.1073/pnas.1800305115.

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Soils support terrestrial ecosystem function and therefore are critical urban infrastructure for generating ecosystem services. Urbanization processes modify ecosystem function by changing the layers of soils identified as soil horizons. Soil horizons are integrative proxies for suites of soil properties and as such can be used as an observable unit to track modifications within soil profiles. Here, in an analysis of 11 cities representing 10 of the 12 soil orders, we show that urban soils have ∼50% fewer soil horizons than preurban soils. Specifically, B horizons were much less common in urba
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Perdomo, Carolina V., Lidiane C. Nogueira, Miriam G. Miguel, and Francisco S. B. Ladeira. "Analysis of water retention in soil horizons of two open trenches on a slope of Serra do Mar, Brazil, susceptible to landslides." MATEC Web of Conferences 337 (2021): 03015. http://dx.doi.org/10.1051/matecconf/202133703015.

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This research presents and analyzes the results of Soil Water Characteristic Curves (SWCC) for the soil horizons (A, B and C) of two different trenches (TR3 and TR7) opened along a slope located in the Serra da Mar mountain range, Brazil. Microaggregations were observed in soil horizons of both trenches, which changed the textural classification of the soils. TR7 showed more macropores than TR3, especially on horizon C. Unimodal SWCC were obtained for soils of the horizon A for both trenches. Instead, bimodal SWCC were obtained for soils of the deeper horizons (B and C). All soil horizons show
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Donald, Richard G., Darwin W. Anderson, and John W. B. Stewart. "The distribution of selected soil properties in relation to landscape morphology in forested Gray Luvisol soils." Canadian Journal of Soil Science 73, no. 2 (1993): 165–72. http://dx.doi.org/10.4141/cjss93-019.

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Properties of Gray Luvisol soils were examined in relation to landscape position in a boreal setting in Saskatchewan. The thickness of the organic, Ae and Bt horizons, the pH of the Ae, depth to carbonates and the percent clay in the Bt horizon were determined on samples taken from 80 profiles on a 70 × 56-m grid. At each sample location the landform element was described as one of eight elements based on the gradient, profile curvature and plan curvature. The results show that the distribution of soil properties varied as a function of landscape morphology and moisture regime. In general, the
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Podrebarac, Frances A., Sharon A. Billings, Kate A. Edwards, Jérôme Laganière, Matthew J. Norwood, and Susan E. Ziegler. "Soil profile connectivity can impact microbial substrate use, affecting how soil CO<sub>2</sub> effluxes are controlled by temperature." Biogeosciences 18, no. 16 (2021): 4755–72. http://dx.doi.org/10.5194/bg-18-4755-2021.

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Abstract. Determining controls on the temperature sensitivity of heterotrophic soil respiration remains critical to incorporating soil–climate feedbacks into climate models. Most information on soil respiratory responses to temperature comes from laboratory incubations of isolated soils and typically subsamples of individual horizons. Inconsistencies between field and laboratory results may be explained by microbial priming supported by cross-horizon exchange of labile C or N. Such exchange is feasible in intact soil profiles but is absent when soils are isolated from surrounding depths. Here
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Alba, José Maria Filippini, Carlos Alberto Flores, and Alberto Miele. "Relationships Between A and B/A2 Horizons of Three Soils in the Context of Viticulture." Journal of Agricultural Studies 9, no. 1 (2021): 440. http://dx.doi.org/10.5296/jas.v9i1.18320.

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The purpose of this study was a comparison of soil parameters among superficial and sub-superficial horizons of three representative type of soils in Vale dos Vinhedos, Brazil, aiming Viticulture in general, but Precision Viticulture (PV) management as specific focus. Basic aspects of Viticulture or PV are still discussed, by instance, sampling procedures, influence of pedology on quality of wine or methods for defining the management zones. Samples were collected according to each horizon, superficial (0-20 cm in depth) or sub-superficial (&gt;40 cm in depth), that is, A (all soils), A2 (Neos
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Hendershot, William H. "A Comparison of some Upland and Valley Soils in the Ungava-Labrador Peninsula." Géographie physique et Quaternaire 38, no. 3 (2007): 243–56. http://dx.doi.org/10.7202/032566ar.

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ABSTRACT Thirteen soil profiles from northern Québec and Labrador, Canada, near the northern tree-line, were sampled and analysed. Five of these, located on poorly to imperfectly drained sites, are strongly cryoturbated soils with permafrost at a shallow depth. Below the surface horizon they have very uniform profile distributions of pH, carbon and extractable iron and aluminum due to the active mixing of the horizons. The eight soils from well-drained sites have profiles similar to those of soils in similar settings in more temperate climatic regions. One of these, developed in one of the mos
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Weitzman, Julie N., and Jason P. Kaye. "Nitrate retention capacity of milldam-impacted legacy sediments and relict A horizon soils." SOIL 3, no. 2 (2017): 95–112. http://dx.doi.org/10.5194/soil-3-95-2017.

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Abstract. While eutrophication is often attributed to contemporary nutrient pollution, there is growing evidence that past practices, like the accumulation of legacy sediment behind historic milldams, are also important. Given their prevalence, there is a critical need to understand how N flows through, and is retained in, legacy sediments to improve predictions and management of N transport from uplands to streams in the context of climatic variability and land-use change. Our goal was to determine how nitrate (NO3−) is cycled through the soil of a legacy-sediment-strewn stream before and aft
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Dmytruk, Yuri. "Analysis of morphometric features of soil profiles to rating their evolution." Visnyk of the Lviv University. Series Geography, no. 44 (November 28, 2013): 91–98. http://dx.doi.org/10.30970/vgg.2013.44.1204.

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We studied the soil of different ages of chronological catenas at stationary Precarpathian and PrutDniester interfluvial. The obtained results of the morphometric features of the background and buried soils extend the capabilities for the interpretation of their evolution. Thus more soundly use of absolute values of morphometric parameters of genetic soil horizons. We showed, that the thickness of humus horizons and first of all the background soil profile generally, during the time after burial of soil increased. This is due to an increase in humidity of the climate in the last 1000 years. Ke
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Tikhonovich, I. A., T. I. Chernov, A. D. Zhelezova, A. K. Tkhakakhova, E. E. Andronov, and O. V. Kutovaya. "TAXONOMIC STRUCTURE OF PROKARYOTIC COMMUNITIES IN SOILS OF DIFFERENT BIOCLIMATIC ZONES." Dokuchaev Soil Bulletin, no. 95 (November 1, 2018): 125–53. http://dx.doi.org/10.19047/0136-1694-2018-95-125-153.

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Using high-throughput sequencing, we performed a full-profile analysis of the taxonomic structure and diversity of prokaryotic communities of zonal soil series: sod-podzolic, dark gray, typical chernozem, brown soil, meadow-chestnut soil and solonets. Phyla Acidobacteria, Actinobacteria, Bacteroidetes, Chloroflexi, Firmicutes, Gemmatimonadetes, Planctomycetes, Proteobacteria and Verrucomicrobia formed up to 95% of prokaryotic communities in all studied soil horizons. Phyla Proteobacteria and Actinobacteria and archaeal phylum Thaumarchaeota dominated in all soils. We revealed the trends of cha
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Dissertations / Theses on the topic "Soil horizons"

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Pereira, Osvaldo José Ribeiro. "Mapping soil organic carbon storage in deep soil horizons of Amazonian Podzols." Universidade de São Paulo, 2016. http://www.teses.usp.br/teses/disponiveis/64/64135/tde-14062016-113621/.

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The Podzols of the world are divided into intra-zonal and zonal according to then location. Zonal Podzols are typical for boreal and taiga zone associated to climate conditions. Intra-zonal podzols are not necessarily limited by climate and are typical for mineral poor substrates. The Intra-zonal Podzols of the Brazilian Amazon cover important surfaces of the upper Amazon basin. Their formation is attributed to perched groundwater associated to organic matter and metals accumulations in reducing/acidic environments. Podzols have a great capacity of storing important amounts of soil organic car
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Simonsson, Magnus. "Mechanisms controlling the solubility of aluminium in B horizons of podzolized soils /." Uppsala : Swedish Univ. of Agricultural Sciences (Sveriges lantbruksuniv.), 1999. http://epsilon.slu.se/avh/1999/91-576-5711-4.pdf.

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Kothawala, Dolly N. "Controls on the soil solution partitioning of dissolved organic carbon and nitrogen in the mineral horizons of forested soils." Thesis, McGill University, 2009. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=115565.

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Note:<br>The soil-solution partitioning of dissolved organic carbon (DOC) withinmineral soil horizons is primarily controlled by processes of adsorption and desorption. These abiotic processes largely occur within a short equilibration time of seconds to minutes, which generally occur faster than microbial processes. To characterise the adsorption of DOC to mineral soils, I used the Langmuir adsorption isotherm, which holds several advantages to the commonly used linear initial mass (IM) isotherm. One advantage to using the Langmuir isotherm is anestimation of the maximum DOC adsorption capaci
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Kothawala, Dolly N. 1972. "Controls on the soil solution partitioning of dissolved organic carbon and nitrogen in the mineral horizons of forested soils." Thesis, McGill University, 2009. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=115858.

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The soil-solution partitioning of dissolved organic carbon (DOC) within mineral soil horizons is primarily controlled by processes of adsorption and desorption. These abiotic processes largely occur within a short equilibration time of seconds to minutes, which generally occur faster than microbial processes. To characterise the adsorption of DOC to mineral soils, I used the Langmuir adsorption isotherm, which holds several advantages to the commonly used linear initial mass (IM) isotherm. One advantage to using the Langmuir isotherm is an estimation of the maximum DOC adsorption capacity (Qma
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Wardinski, Katherine Mary. "Dissolved Organic Matter Sources from Soil Horizons with Varying Hydrology and Distance from Wetland Edge." Thesis, Virginia Tech, 2021. http://hdl.handle.net/10919/104933.

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Understanding hydrologic controls on carbon accumulation and export within geographically isolated wetlands (GIW) has implications for the success of wetland restoration efforts intended to produce carbon sinks. However, little is known about how hydrologic connectivity along the aquatic-terrestrial interface in GIW catchments influences carbon dynamics, particularly regarding dissolved organic matter (DOM) transport and transformation. The organic matter (carbon) that accumulates in wetland soils may be released into water, generating DOM. DOM is mobile and reactive, making it influential to
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Blaud, Aimeric. "Responses of microbial communities to atmospheric nitrogen deposition within different soil horizons in High Arctic tundra." Thesis, University of Sheffield, 2012. http://etheses.whiterose.ac.uk/2759/.

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Arctic environments are subject to acute nitrogen deposition events, in which 40% or more of annual atmospheric N input can be deposited as acidic rainfall in less than one week. The overall aim of this research was to investigate the impact of acute N deposition events upon soil microbial communities in High Arctic tundra. A plot scale field experiment, established on the High Arctic tundra (Ny-Ålesund, Svalbard), and a microcosm experiment, were used to simulate acute N deposition over the summer by the application of NH4NO3 solution at ~pH 4, at rates of 0.4, 4 and 12 kg N ha-1 yr-1. Chang
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Thomsen, Frida. "A laboratory study on the immobilisation of inorganic chlorine in soil." Thesis, Linköping University, The Tema Institute, 2006. http://urn.kb.se/resolve?urn=urn:nbn:se:liu:diva-7164.

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<p>Inorganic chlorine (Clinorg) is generally considered to be inert and has been used as a tracer for groundwater movements. This assumption is thereby fundamental for current knowledge about soil biogeochemistry. However, recent work showed that Clinorg can be retained, i.e. immobilised, in soil, which contradicts the previous assumptions. The aim of this laboratory study was to investigate if the processes that immobilise Clinorg in soil are affected by molecular oxygen (O2), and if the immobilisation occurs in the top soil layer only or also further down were the soil structure is different
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Weiglein, Tyler Lorenz. "A Continental-Scale Investigation of Factors Controlling the Vulnerability of Soil Organic Matter in Mineral Horizons to Decomposition." Thesis, Virginia Tech, 2019. http://hdl.handle.net/10919/101987.

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Soil organic matter (SOM) is the largest terrestrial pool of organic carbon (C), and potential carbon-climate feedbacks involving SOM decomposition could exacerbate anthropogenic climate change. Despite the importance of SOM in the global C cycle, our understanding of the controls on SOM stabilization and decomposition is still developing, and as such, SOM dynamics are a source of major uncertainty in current Earth system models (ESMs), which reduces the effectiveness of these models in predicting the efficacy of climate change mitigation strategies. To improve our understanding of controls on
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Holland, Anne E. "Organic lamellae in the eluvial horizons of podzols : a field study of the distribution of a morphological feature in the soil landscape." Thesis, University of Reading, 1989. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.329721.

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Lopes, Josiane Millani. "Caracterização e evolução das substâncias húmicas de horizontes espódicos na planície costeira do estado de São Paulo." Universidade de São Paulo, 2011. http://www.teses.usp.br/teses/disponiveis/11/11140/tde-10022011-100856/.

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A evolução da planície costeira do Estado de São Paulo foi influenciada por eventos de transgressões e regressões do mar durante o Quaternário e suas características resultam da interação da dinâmica dos processos geológicogeomorfológicos que agiram continuamente durante esses eventos. Os solos de maior ocorrência nesse ambiente, genericamente chamado de restinga, são os Espodossolos, caracterizados pela presença de horizonte espódico (Bh ou Bhm). São poucos os estudos científicos relacionadas à gênese destes solos em regiões tropicais, assim como há poucos estudos detalhados avaliando as cara
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Books on the topic "Soil horizons"

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Bridges, E. M. Soil horizon designations. International Soil Reference and Information Centre, 1990.

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FitzPatrick, Ewart Adsil. Soil horizon, designation, and classification: A coordinate system for defining soil horizons and their use as the basic elements in soil classification for different purposes. International Soil Reference and Information Centre (IRIC), 1988.

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Bernabé, M. Nieves. Designación de los horizontes y capas del suelo: Evolución histórica y localización en la Comunidad de Madrid. Consejería de Cooperación, 1992.

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Veress, Benjamin. Horizons in earth science research. Nova Science Publishers, 2010.

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Mallawatantri, A. P. Pesticide sorption and degradation in macropores and soil horizons in the Palouse. State of Washington Water Research Center, 1994.

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Horizontes de sol: Cuentos tempranos. 2nd ed. San Marcos, 2007.

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Be lo Horizonte: O fértil solo humano = the fertile human soil. Salamandra, 1997.

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Massachusetts, Inc AMEC. Phase III remedial action plan: Phase IV remedy implementation plan : sediment portion of the Former Everett Staging Yard Disposal Site : 1 Horizon Way, Everett, Massachusetts. AMEC Massachusetts, Inc., 2017.

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Inc, GZA GeoEnvironmental. Revised release abatement measure (RAM) plan modification: Construction-related remediation activities former Everett Staging Yard, 1 Horizon Way, Everett, Massachusetts. GZA Geoenvironmental, Inc., 2016.

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Inc, GZA GeoEnvironmental. Release abatement measure status report no. 2: Pre-construction remediation activities (former) Everett Staging Yard, 1 Horizon Way, Everett, Massachusetts. GZA Geoenvironmental, Inc., 2016.

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Book chapters on the topic "Soil horizons"

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Thoresen, Kimberley, Kimberley L. Chandler, and William Mary. "Soil Horizons." In The Earth Beneath Our Feet. Routledge, 2021. http://dx.doi.org/10.4324/9781003238775-16.

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Bockheim, James G. "Calcic and Petrocalcic Horizons." In Soil Geography of the USA. Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-06668-4_12.

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Bockheim, James G. "Gypsic and Petrogypsic Horizons." In Soil Geography of the USA. Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-06668-4_17.

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Bockheim, James G. "Ortstein and Placic Horizons." In Soil Geography of the USA. Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-06668-4_18.

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Toland, Alexandra, and Gerd Wessolek. "Merging Horizons—Soil Science and Soil Art." In Soil and Culture. Springer Netherlands, 2009. http://dx.doi.org/10.1007/978-90-481-2960-7_4.

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Bockheim, James G., and Alfred E. Hartemink. "Diagnostic Horizons and Soil Taxa." In World Soils Book Series. Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-52144-2_6.

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Trudgill, Steven T. "Soil Processes and their Significance." In Horizons in Physical Geography. Macmillan Education UK, 1987. http://dx.doi.org/10.1007/978-1-349-18944-1_12.

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Bockheim, James G. "Argillic, Kandic, and Natric Horizons." In Soil Geography of the USA. Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-06668-4_11.

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Beaudette, D. E., P. Roudier, and J. Skovlin. "Probabilistic Representation of Genetic Soil Horizons." In Progress in Soil Science. Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-28295-4_18.

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Tan, Sister Christine. "2. Preface to Part II; The Foreign Missionary Enters Filipino Soil: Recall the Disconnections." In Grassroot Horizons. Practical Action Publishing, 1995. http://dx.doi.org/10.3362/9781780445052.002.

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Conference papers on the topic "Soil horizons"

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Treese, Daniel P., Shirley E. Clark, and Katherine H. Baker. "Nutrient Leaching from Disturbed Soil Horizons." In World Environmental and Water Resources Congress 2010. American Society of Civil Engineers, 2010. http://dx.doi.org/10.1061/41114(371)302.

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Popov, Leonid, Aureliu Overcenco, and Stela Curcubat. "Considerațiuni privind folosirea polipedonului în aprecierea răspîdirii spațiale a solurilor." In Starea actuală a componentelor de mediu. Institute of Ecology and Geography, Republic of Moldova, 2019. http://dx.doi.org/10.53380/9789975315593.11.

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The specificity of zonal pedogenesis factors and their influence on the horizon thickness in the soil profile contributes to the formation of specific characters for each horizon. A clear example can be observed in the interaction between pedogenesis and hydrology, where the illuvial and spontaneous processes move soil-clay minerals, oxides, soil carbon, carbonates and other compounds into the soil profile. Such reciprocal links allow the application of the statistical analysis to assess the variability of the horizons thickness and the prognosis of their spatial spread in relation to the fact
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Berggren, Mark, Robert Zubrin, Peter Jonscher, and James Kilgore. "Lunar Soil Particle Separator." In 49th AIAA Aerospace Sciences Meeting including the New Horizons Forum and Aerospace Exposition. American Institute of Aeronautics and Astronautics, 2011. http://dx.doi.org/10.2514/6.2011-436.

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Kleinhenz, Julie, and Allan Wilkinson. "ISRU Soil Mechanics Vacuum Facility: Soil Bin Preparation and Simulant Strength Characterization." In 50th AIAA Aerospace Sciences Meeting including the New Horizons Forum and Aerospace Exposition. American Institute of Aeronautics and Astronautics, 2012. http://dx.doi.org/10.2514/6.2012-359.

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MOROZ, Hryhorii. "AGROPEDOGENIC TRANSFORMATION OF PHYSICAL PROPERTIES OF SOILS OF MEDIUM-DRY STEPPE PEDO-ECOTONE IN THE NORTHWEST OF THE BLACK SEA REGION." In RURAL DEVELOPMENT. Aleksandras Stulginskis University, 2018. http://dx.doi.org/10.15544/rd.2017.184.

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The anthropogenic transformation of soil physical properties of the transition stripe from the dry to the middle steppe in the Northwest of the Black Sea region is considered and analyzed on the basis of comparison of indicators characterizing the properties of the cultivable and subcultivable horizons. The signs of negative influence of agricultural use on the most important indices of physical properties of soils are investigated. Significant degradation of the physical properties of the arable horizons (in comparison with tillable and subcultivable horizons), as well as deterioration of the
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Qiu, Lin, and Anbo Li. "Automated keys of soil diagnostic horizons based on case-based reasoning." In 2014 Third International Conference on Agro-Geoinformatics. IEEE, 2014. http://dx.doi.org/10.1109/agro-geoinformatics.2014.6910638.

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Robins, Colin R. "PALEOENVIRONMENTAL ANALYSIS OF (PETRO)CALCIC SOIL HORIZONS IN THE MOJAVE DESERT." In Keck Proceedings. Keck Geology Consortium, 2019. http://dx.doi.org/10.18277/akrsg.2019.32.13.

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Conley, Ethan W. "MORPHOLOGY AND GENESIS OF PEDOGENIC OOIDS IN CALCIC AND PETROCALCIC SOIL HORIZONS." In Keck Proceedings. Keck Geology Consortium, 2019. http://dx.doi.org/10.18277/akrsg.2019.32.14.

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Sudduth, K., N. Kitchen, B. Myers, and S. Drummond. "Estimating Depth to Argillic Soil Horizons using Apparent Electrical Conductivity Response Functions." In 22nd EEGS Symposium on the Application of Geophysics to Engineering and Environmental Problems. European Association of Geoscientists & Engineers, 2009. http://dx.doi.org/10.3997/2214-4609-pdb.157.sageep093.

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Sudduth, Kenneth A., Newell R. Kitchen, D. Brenton Myers, and Scott T. Drummond. "Estimating Depth to Argillic Soil Horizons Using Apparent Electrical Conductivity Response Functions." In Symposium on the Application of Geophysics to Engineering and Environmental Problems 2009. Environment and Engineering Geophysical Society, 2009. http://dx.doi.org/10.4133/1.3176776.

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Reports on the topic "Soil horizons"

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Wells, Aaron, Tracy Christopherson, Gerald Frost, et al. Ecological land survey and soils inventory for Katmai National Park and Preserve, 2016–2017. National Park Service, 2021. http://dx.doi.org/10.36967/nrr-2287466.

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This study was conducted to inventory, classify, and map soils and vegetation within the ecosystems of Katmai National Park and Preserve (KATM) using an ecological land survey (ELS) approach. The ecosystem classes identified in the ELS effort were mapped across the park, using an archive of Geo-graphic Information System (GIS) and Remote Sensing (RS) datasets pertaining to land cover, topography, surficial geology, and glacial history. The description and mapping of the landform-vegetation-soil relationships identified in the ELS work provides tools to support the design and implementation of
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Gebhart, Dick L., H. A. Torbert, and Michael Hargrave. Identifying Military Impacts on Archaeological Deposits Based on Differences in Soil Organic Carbon and Chemical Elements at Soil Horizon Interfaces. Defense Technical Information Center, 2012. http://dx.doi.org/10.21236/ada559158.

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Garrett, R. G. The distribution of cadmium in a horizon soils in the prairies of Canada and adjoining United States. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1994. http://dx.doi.org/10.4095/193656.

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Matheis, G., and A. Utke. Regional geochemical mapping in the tropical environment: bedrock reflection of Precambrian volcanosedimentary sequences in B-horizon soil strata: case studies from Nigeria/West Africa. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1993. http://dx.doi.org/10.4095/193272.

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You might also be interested in the extended bibliographies on the topic 'Soil horizons' for particular source types:
Journal articles Dissertations / Theses Books
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