Academic literature on the topic 'Soil profile'

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Journal articles on the topic "Soil profile"

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Salh, Qadri, Zhino Abdalla, Khasraw Rashid, and Shuela Sheikh-Abdullah. "Assessment of Fe, Ni, Zn, Cu, Cr, and Cd Migration in Soil Profiles Affected by Open Dump Leachate in Tanjero area." Journal of Zankoy Sulaimani - Part A 25, no. 2 (2023): 12. http://dx.doi.org/10.17656/jzs.10917.

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The properties of an open dump area are important to the application of the elements to the soils and their migrations through soil depth; therefore this study was investigated to evaluate the migration of elements in an open dump area. Soil samples were taken from three soil profiles, one of them was at an open dump site, and the second and third profiles were taken at different distances from the open dump site. In total eighteen soil sample were collected. Some soil physical and chemical properties were determined for each horizon. Total concentrations of Fe, Ni, Zn, Cu, Cr, and Cd were det
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Mad Said, Mohd Jazlan, Adnan Zainorabidin, and Aziman Madun. "Soil Velocity Profile on Soft Soil Using Seismic Refraction." Applied Mechanics and Materials 773-774 (July 2015): 1549–54. http://dx.doi.org/10.4028/www.scientific.net/amm.773-774.1549.

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Soil velocity profile often used as subsurface characterization by using geophysical technic. Seismic refraction is one of geophysical technique to determine primary wave (p-wave) velocity of soil profile. In this paper, seismic refraction technique has been performed on two different types of soft soil (peat soil and RECESS clay) for comparison of its p-wave velocity soil profile. From p-wave velocity soil profile comparison, its show the peat soil has soil velocity range from 211 m/s – 534 m/s at depth of 0 – 4 m while the soft clay show soil velocity range from 248 m/s – 1842 m/s at depth o
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O'Brien, Bernard John. "The Use of Natural and Anthropogenic 14C to Investigate the Dynamics of Soil Organic Carbon." Radiocarbon 28, no. 2A (1986): 358–62. http://dx.doi.org/10.1017/s0033822200007463.

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Radiocarbon has been measured in two soil profiles, one of which has been covered by a building since 1956. A comparison of the Δ14C values in horizons of each profile gives an estimate of the total input of atom bomb 14C into the soil profile. From the Δ14C and carbon density profile data, the carbon input rates, respiration rates, and diffusivity are calculated. The lack of vegetation on one soil affects the mobility and the respiration rate of the soil carbon in that soil. The data from this soil profile are also used to check the assumption, used in previous analyses, that there is a unifo
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Bowo, Cahyoadi, Wahyu Hidayat, and Victor B. Asio. "Distribution of soil minerals along the toposequence of Hyang-Argopuro Volcanic Mountain, Jember, Indonesia." EURASIAN JOURNAL OF SOIL SCIENCE (EJSS) 13, no. 2 (2024): 167–78. http://dx.doi.org/10.18393/ejss.1424885.

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The study was conducted in the Hyang-Argopuro volcanic mountain in Jember, Indonesia, with the aim of assessing the distribution of soil minerals along a toposequence and their relationship to soil genesis. Three soil profiles representing the upper, middle, and lower slopes of the toposequence were analyzed. The results revealed that the predominant sand minerals in the soils are opaque minerals, weatherable minerals, amphibole groups, and ferromagnesian minerals. The presence of magnetite, primarily found in the soil profile on the upper slope, suggests the effect of the well-drained topogra
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Skvortsova, E. B., K. N. Abrosimov, and K. A. Romanenko. "CHANGES IN MICROMORPHOMETRIC PARAMETERS OF VOIDS ALONG THE PROFILE OF ZONAL SOILS IN EUROPEAN RUSSIA." Dokuchaev Soil Bulletin, no. 78 (May 1, 2015): 42–58. http://dx.doi.org/10.19047/0136-1694-2015-78-42-58.

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The soils are distinguished by the presence and the profile distribution pattern of such pedogenic parameters as the organic matter content, available pedofeatures, structural state of the soil mass, etc. They differ in the organization of the pore space throughout the soil profile as well. Under discussion are results of computer micromorphometric analysis of fine macropores d = 0.2-2.0 mm in thin sections of vertical orientation from samples taken in genetic horizons of podzolic, soddy podzolic, gray forest soils and chernozems at the territory of European Russia. The profile changes in void
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Silva, Jucirema Ferreira da, Miguel Ferreira Neto, Jeane Cruz Portela, et al. "Soil Classification Based on Local and Scientific Knowledge in an Irrigated District in the Semi-Arid Region of Brazil." Land 13, no. 10 (2024): 1559. http://dx.doi.org/10.3390/land13101559.

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Ethnopedology offers a unique opportunity to recognize and highlight invaluable local soil knowledge (LSK). We aimed to classify three soil profiles in a Brazilian irrigated district with salt-affected soils based on smallholder farmers’ LSK and scientific knowledge. The study occurred in the Baixo-Açu irrigation district in Brazil’s semi-arid region. Three soil profiles were characterized by researchers (etic approach) and farmers (emic approach) in the following areas: P1 profile (area under banana cultivation), P2 profile (fallow area), and P3 profile (native forest area). Smallholder farme
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Rokich, Deanna P., Kathy A. Meney, Kingsley W. Dixon, and K. Sivasithamparam. "The impact of soil disturbance on root development in woodland communities in Western Australia." Australian Journal of Botany 49, no. 2 (2001): 169. http://dx.doi.org/10.1071/bt00015.

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The impact of soil disturbance of the Banksia woodland soil profile and particularly the effect of different reconstructed soil profiles (overburden profile, white profile and yellow profile) and soil ripping within rehabilitation sites, was investigated in terms of root development and architecture for eight species that are key structural elements in Banksia woodland. The aim was to determine the soil environment best suited for root development and architecture likely to contribute to high seedling survival in post-mined sites. Root development and architecture differed significantly betwee
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Smaga, I. S. "Diagnostic problems of elementary soil processes and profile-differentiated soils of the Precarpathian region." Fundamental and Applied Soil Science 17, no. 1-2 (2016): 40–48. http://dx.doi.org/10.15421/041604.

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Present condition, scientific concepts and ways of further development of diagnosis problem of elementary soil processes and genetic nature profiled-differentiated gleyed soils of the Pre-Carpathian region, known as brownish-podzolic, brownsoil-podzolic and sod-podzolic, based on stable indicators of soil properties are studied. Eluvial-illuvial differentiation nature of the soil profile of the studied soils is founded. The aim of research was to develop criteria for the diagnosis of elementary soil processes and genetic nature profiled-differentiated soil deposits of Ciscarpathia and discover
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Perez-Rodriguez, JL, C. Maqueda, P. Rodriguezrubio, and MCJ Deharo. "Occurrence of talc in soils with high iron content from the south-west of Spain." Soil Research 34, no. 5 (1996): 635. http://dx.doi.org/10.1071/sr9960635.

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The mineralogy of the clay fractions of 2 soil profiles classified as an Alfic Dystric Eutrochrept (Soil I) and a Xerochreptic Haploxeralf (Soil II) has been determined. A notable feature of these soils is the presence of talc and the high iron content as goethite, hematite, lepidocrocite, and maghemite. Talc was the most abundant non-iron mineral of the clay fraction of Soil II. In Soil I, talc occurs as a residual phase from the parent material with its persistence in the profile aided by coatings of iron oxides, which inhibit further weathering. In these soils there is a high proportion of
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Hidayat, Wahyu, Dyah Tjahyandari Suryaningtyas, and Budi Mulyanto. "Soil fertility based on mineralogical properties to support sustainable agriculture management." SAINS TANAH - Journal of Soil Science and Agroclimatology 21, no. 1 (2024): 95. http://dx.doi.org/10.20961/stjssa.v21i1.85502.

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<p>Detailed information on soil mineral composition has been crucial in providing the basis for designing sustainable agricultural practices, as this information offers long-term insights into natural soil fertility. This research aimed to further investigate the characteristics of soil mineral composition as a basis for managing soil fertility. Three soil profiles representing three different parent materials have been examined in the field, and soil samples have been collected for laboratory analysis. Profile 1 originates from the Raung Volcano Rock Formation (Qhvr). Profile 2 originat
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Dissertations / Theses on the topic "Soil profile"

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Chung, Sun-Ok. "On-the-go soil strength profile sensor /." free to MU campus, to others for purchase, 2004. http://wwwlib.umi.com/cr/mo/fullcit?p3137684.

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Malvajerdi, Ahmad Sharifi. "Development of a soil compaction profile sensor." Thesis, Cranfield University, 2004. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.414666.

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Hancock, Steven J. "Geostatistics in soil profile interpretation for irrigated Riverland properties /." Title page, contents and abstract only, 1995. http://web4.library.adelaide.edu.au/theses/09SB/09sbh235.pdf.

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Udukumburage, Rajitha Shehan. "Investigation of climatic-induced ground responses in expansive soils." Thesis, Queensland University of Technology, 2020. https://eprints.qut.edu.au/198195/1/Rajitha%20Shehan_Udukumburage_Thesis.pdf.

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This thesis presents a practical approach for geotechnical practitioners to investigate the climatic-induced ground responses in expansive soils. The method is based on a novel long-term operable instrumented soil column (ISC). This research investigated the applicability of the current displacement models to the Australian context. As a result, the structural damages and maintenance costs due to cracking of light-weight structures founded on such soils can be minimised, and more importantly, the hazards to human lives can be prevented by improved decisions.
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Sanchez, Pedro Andrade. "Design, development, and field evaluation of a soil compaction profile sensor /." For electronic version search Digital dissertations database. Restricted to UC campuses. Access is free to UC campus dissertations, 2004. http://uclibs.org/PID/11984.

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Nussberger, Mathis. "Soil moisture determination with TDR: single-rod probes and profile reconstruction algorithms /." Zürich, 2005. http://e-collection.ethbib.ethz.ch/show?type=diss&nr=15965.

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Jessett, Clifford Alan. "Investigation of the liquefaction of a soil profile using in situ tests." Thesis, City University London, 1992. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.316399.

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Zou, Ze-Yuan. "Determination of flow and transport properties in a deep unsaturated soil profile." Diss., The University of Arizona, 1999. http://hdl.handle.net/10150/284526.

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Three goals of this research were: (1) to study the movement of a non-reactive tracer (bromide) and of water through non-aggregated fine sand, with low clay (1.2%) and organic matter content (<1%); 2) to develop an inverse method for estimating the hydraulic properties of unsaturated soil from intermediate- and field-scale infiltration data; and (3) to develop a transient in-situ method for calibrating the neutron probe. All three goals of this research are crucial for understanding and determining water and solute transport at the intermediate to field scale. The field research was conducted
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HAMED, LAMY MAMDOH MOHAMED. "NITROGEN BALANCE IN SOIL PROFILE AS AFFECTED BY DIFFERENT SOIL TYPE, SOIL WATER REGIMES, NITROGEN RATE AND APPLICATION METHODS USING 15N TRACER TECHNIQUE." Doctoral thesis, Università degli Studi di Milano, 2014. http://hdl.handle.net/2434/232140.

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The interaction effect of “Soil type, Soil water regime, Nitrogen fertilizer application Rates and Timing” on Nitrogen balancein soil were studied; in terms of nitrogen gained by plant portions, remained in soil, and losses through different ways under wheat (Triticum aestivum L. Giza 168), in order to identify the most proper and effective combinations of above-studied variables that provides a satisfactory grain wheat yield and minimizes the use of chemical nitrogen fertilizers, to save the surrounding environment and to achieve good water saving. Two fields of experiments were carried out
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Timmenga, Hubert J. "The transport of mineral and organic matter into the soil profile by Lumbricus rubellus Hoffmeister." Thesis, University of British Columbia, 1987. http://hdl.handle.net/2429/27551.

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The biology and ecology of the earthworm Lumbricus rubellus Hoffmeister, 1843, and its effects on the turn-over of organic matter and soil are not well known. To gather this information, the ingestion and egestion rates were measured using a litterbag technique and the transport of organic matter was quantified with a newly developed method, using soil columns to which ¹⁴C labelled plant material was added. The feeding habits of the worm were positively influenced by temperature in wet soils (> -15m of water) and were negatively influenced in dry soil (< -15 m of water). The total egestion ra
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Books on the topic "Soil profile"

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Remmelzwaal, A. Botswana soil database: Guidelines for soil profile description. Food and Agriculture Organization of the United Nations, 1988.

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C, Tijmons J., ed. Manual for soil profile description. Soil Survey Unit, Research Branch, Dept. of Agriculture, 1985.

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Mbuvi, J. P. Explanations and profile description to reconnaissance soil survey of the upper Ewaso Ng'iro basin (Laikipia East and slopes west to north of Mount Kenya). Laikipia Research Programme, Natural Resource Monitoring, Modelling, and Management, 1994.

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Habiba, Hasan, ed. Syed Hasan Nasir: A profile. Habiba Hasan, 1990.

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Bundi, D. N. Nakuru report, 1987: Soil conservation profile in Molo Division. Ministry of Agriculture, Agriculture Engineering Division, Soil & Water Conservation Branch, 1988.

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Ndege, Henry O. Narok report, 1987: Socio-economic profile. Ministry of Agriculture, Agriculture Engineering Division, Soil & Water Conservation Branch, 1987.

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Sheppard, Marsha I. Strategy for modelling soil erosion and soil profile development in a landscape for environmental impact assessments. AECL, Whiteshell Laboratories, 1995.

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W, Markewich Helaine, and United States. Soil Conservation Service., eds. A Guide for using soil and weathering profile data in chronosequence studies of the coastal plain of the eastern United States. U.S. G.P.O., 1989.

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A, Williams Robert, Geological Survey (U.S.), and National Earthquake Hazards Reduction Program (U.S.), eds. High-resolution surface-seismic imaging techniques for NEHRP soil profile classifications and earthquake hazard assessments in urban areas. U.S. Geological Survey, 1997.

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1958-, Williams Robert A., Geological Survey (U.S.), and National Earthquake Hazards Reduction Program (U.S.), eds. High-resolution surface-seismic imaging techniques for NEHRP soil profile classifications and earthquake hazard assessments in urban areas. U.S. Geological Survey, 1997.

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Book chapters on the topic "Soil profile"

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Blake, George R., Gary C. Steinhardt, X. Pontevedra Pombal, et al. "Profile." In Encyclopedia of Soil Science. Springer Netherlands, 2008. http://dx.doi.org/10.1007/978-1-4020-3995-9_466.

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Lindbo, David, Randy Miles, DeAnn Presley, and Nora E. Ransom. "Soil Profile Descriptions." In Soil Science Step-by-Step Field Analysis. American Society of Agronomy and Soil Science Society of America, 2015. http://dx.doi.org/10.2136/2008.soilsciencestepbystep.c2.

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Odgers, Nathan P., Alex B. McBratney, and Florence Carré. "Soil Profile Classes." In Pedometrics. Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-63439-5_9.

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Blake, George R., Gary C. Steinhardt, X. Pontevedra Pombal, et al. "Profile, Physical Modification." In Encyclopedia of Soil Science. Springer Netherlands, 2008. http://dx.doi.org/10.1007/978-1-4020-3995-9_467.

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Paltseva, Anna. "What Is a Soil Profile?" In The Urban Soil Guide. Springer Nature Switzerland, 2024. http://dx.doi.org/10.1007/978-3-031-50777-9_2.

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Eck, H. V., and P. W. Unger. "Soil Profile Modification for Increasing Crop Production." In Advances in Soil Science. Springer New York, 1985. http://dx.doi.org/10.1007/978-1-4612-5046-3_2.

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Demattê, José A. M. "From Profile Morphometrics to Digital Soil Mapping." In Progress in Soil Science. Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-28295-4_24.

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Roudier, Pierre, Andrew Manderson, and Carolyn Hedley. "Advances Towards Quantitative Assessments of Soil Profile Properties." In Progress in Soil Science. Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-28295-4_8.

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Nair, Kodoth Prabhakaran. "General Profile of Current Agricultural Systems." In Intelligent Soil Management for Sustainable Agriculture. Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-15530-8_13.

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Ramke, H. G., and K. Lhotzky. "A New System for the Profile Measurement of Chemical/Physica1 Parameters." In Contaminated Soil ’88. Springer Netherlands, 1988. http://dx.doi.org/10.1007/978-94-009-2807-7_30.

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Conference papers on the topic "Soil profile"

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Narwane, Manisha, and Sheetal Katwe. "Automated Soil Profile Analysis Using Optical Sensors." In 2024 8th International Conference on Computing, Communication, Control and Automation (ICCUBEA). IEEE, 2024. https://doi.org/10.1109/iccubea61740.2024.10775082.

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Khan, Saboor, Abaseen Khan, Nadia Majeed, Nasir Khan, and Saeedullah Mandokhail. "Effect of Shallow Foundation Size on Bearing Capacity of layered Soil: 3D Numerical Simulations." In 14th International Civil Engineering Conference. Trans Tech Publications Ltd, 2025. https://doi.org/10.4028/p-0v8zui.

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The depth of the induced stresses of a rigid foundation known as significant depth, is related to the width of the foundation. The conventional bearing capacity equations can lead to significant inaccuracies if the top layer thickness is less than the significant depth of the foundation. In this study, series of 3D numerical simulation analysis on various sizes of foundation are performed. Two different soil profiles with same top layer underlain by, a) harder soil layers (Soil Profile A) and, b) weaker soil layers (Soil Profile B), were used in this study. The settlement profile showed that t
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Yamnova, Irina, and Galina Chernousenko. "MICROMORPHOLOGICAL FEATURES OF SALT-AFFECTED SOILS FROM THE BAIKAL REGION OF RUSSIA." In 24th SGEM International Multidisciplinary Scientific GeoConference 2024. STEF92 Technology, 2024. https://doi.org/10.5593/sgem2024/3.1/s13.31.

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Micromorphological features of salt-affected soils in the Cis-Baikal and Trans-Baikal regions (south of East Siberia, Russia) are considered. When studying morphogenesis of these soils, pedofeatures of soluble salts and gypsum serve as indicators of modern and former stages of soil formation. Comparative-geographical, micromorphological, and chemical methods have been applied to study soil salinization. Chemical analyses attest to the presence of gypsum and soluble salts in solonchaks of both regions. However, they do not allow us to judge the direction of modern soil salinization processes. M
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Bursik, Lukas, Miroslav Dumbrovsky, and Veronika Sobotkova. "VOLUMETRIC QUANTIFICATION OF SOIL LOSS IN A PART OF THE MUNICIPALITY OF OTNICE IN THE CZECH REPUBLIC." In 24th SGEM International Multidisciplinary Scientific GeoConference 2024. STEF92 Technology, 2024. https://doi.org/10.5593/sgem2024v/3.2/s11.21.

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This paper deals with the volumetric quantification of soil loss. A device called erosion bridge was used for the quantification. It was designed and created at the Institute of Landscape Water Management, Faculty of Civil Engineering, Brno University of Technology. The principle of the measurement with the use of this device is that the needles are lowered onto the terrain surface and their profile copies the terrain profile. A camera attached to the erosion bridge is important, which is used to take photographs of the erosion bridge with the profile of the rill. For the quantification, a dee
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Shishkov, Toma, Emil Dimitrov, and Ekaterina Filchev. "FOREST SOILS FROM SREDNA GORA MOUNTAIN IN BULGARIA." In 24th SGEM International Multidisciplinary Scientific GeoConference 2024. STEF92 Technology, 2024. https://doi.org/10.5593/sgem2024/3.1/s13.29.

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The soils from the central part of Sredna Gora Mountain in Bulgaria were studied aiming to establish the occurrence of contemporal soil forming processes occured in the forest ecosystem. Soils were analyzed to determine the carbon content, the soil organic matter composition and the total soil acidity. The precise soil classification based on the detail morphological diagnostic was carried out. The ecological conditions in forest ecosystem determine the mode of humic substances in the studies soils. Soils are characterized with low degree of humification and considerable amount of organic matt
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Shishkov, Toma, and Emil Dimitrov. "SOIL PROPERTIES OF CHROMIC LUVISOLS FROM KREMIKOVTSI AREA IN SOFIA MUNICIPALITY." In 24th SGEM International Multidisciplinary Scientific GeoConference 2024. STEF92 Technology, 2024. https://doi.org/10.5593/sgem2024/3.1/s13.24.

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The result of the survey carried out on the territory of the Sofia-city municipality is presented, in relation to the application of the Program for the protection, sustainable use and restoration of soils as a limited and non-renewable natural resource. The obtained data on the Chomic Luvisols nearby the area of Kremikovtsi debate the basic physical and chemical soil characteristics. The priority task on the soil protection in the region aimed at the sustainable development, restoration and improvement of the soil resource. To fulfill this aim, samples from soil profile and additional sites f
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Dabkowski, J. "Interpretation of Storage Field Well Casing Surface Potentials." In CORROSION 1987. NACE International, 1987. https://doi.org/10.5006/c1987-87321.

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Abstract The shape of a well casing-to-soil potential gradient surface profile is influenced by many variables. Hence, the interpretation of such field data can be difficult. The paper illustrates how such factors as layered ground resistivity, polarization potential variations with depth, and external interference affect the profiles and, therefore, the interpretation of field data.
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Hou, Zhanfeng, Zhi Chen, Pei Wu, and Zhixiong Lu. "Fractal Analysis of Soil Profile Roughness." In 2010 International Conference on E-Product E-Service and E-Entertainment (ICEEE 2010). IEEE, 2010. http://dx.doi.org/10.1109/iceee.2010.5661225.

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Yan, Xun, Qianqian Pan, and Yunlu Zhao. "Soil Profile Ruler Detection in YOLOv5." In GAIIS 2024: 2024 International Conference on Generative Artificial Intelligence and Information Security. ACM, 2024. http://dx.doi.org/10.1145/3665348.3665403.

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Spirina, V. Z., L. V. Khotskova, and E. A. Zharikova. "PROPERTIES AND ELEMENT COMPOSITION OF SOILS OF THE DENDROLOGICAL TERRITORY OF THE SIBERIAN BOTANICAL GARDEN." In Prirodopol'zovanie i ohrana prirody: Ohrana pamjatnikov prirody, biologicheskogo i landshaftnogo raznoobrazija Tomskogo Priob'ja i drugih regionov Rossii. Izdatel'stvo Tomskogo gosudarstvennogo universiteta, 2020. http://dx.doi.org/10.17223/978-5-94621-954-9-2020-55.

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The properties, content and profile distribution of macroelements in the soils of the dendrological territory of the Siberian Botanical Garden were studied. The nature of the distribution of chemical elements in soil profiles is revealed depending on the intensity of sod, podzolic and glue soil formation processes.
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Reports on the topic "Soil profile"

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Cook, David R. Soil Temperature and Moisture Profile (STAMP) System Handbook. Office of Scientific and Technical Information (OSTI), 2016. http://dx.doi.org/10.2172/1332724.

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Wahl, C., and S. M. Benson. Update to modeling soil selenium concentrations in the shallow soil profile at Kesterson Reservoir Merced County, California. Office of Scientific and Technical Information (OSTI), 1996. http://dx.doi.org/10.2172/431193.

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Wallach, Rony, Tammo Steenhuis, Ellen R. Graber, David DiCarlo, and Yves Parlange. Unstable Flow in Repellent and Sub-critically Repellent Soils: Theory and Management Implications. United States Department of Agriculture, 2012. http://dx.doi.org/10.32747/2012.7592643.bard.

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Water repellency causes unstable wetting fronts that result in water moving in preferential flowpaths through homogeneous soils as well in structured soils where macropores enhance the preferential flow pattern. Water repellency is typically associated with extended water ponding on the soil surface, but we have found that repellency is important even before the water ponds. Preferential flow fingers can form under conditions where the contact angle is less than 90o, but greater than 0o. This means that even when the soil is considered wettable (i.e., immediate penetration of water), water dis
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Guerra, Flávia, Alex Caldera-Ortega, Daniel Tagle Zamora, et al. TUC City Profile: León, Mexico. United Nations University - Institute for Environment and Human Security (UNU-EHS), 2022. http://dx.doi.org/10.53324/gjss3214.

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Economic dynamism has been maintained at the expense of rising socio-environmental issues in León, namely the deterioration of air and water quality, the overexploitation of groundwater sources, soil erosion and contamination, deforestation, loss of biodiversity, urban sprawl and inequality. These issues contribute to, and are worsened by, climate change. Climate governance in León began to materialize in the early 2010s, largely emulating the state’s legal and institutional framework. It has since progressed incrementally with each municipal administration. Nevertheless, mainstreaming of the
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Tran, Thi Hong Van, Bartłomiej Woś, Tomasz Wanic, Marcin Pietrzykowski, and Agnieszka Józefowska. Impact of charcoal and tree species on forest soil recovery after fire disturbance Dataset. Publishing House of the University of Agriculture in Krakow, 2025. https://doi.org/10.15576/repourk/2025.1.1.

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This dataset examines the impact of charcoal and tree species on forest soil recovery post-fire, encompassing soil profile characteristics, particle size distribution (granulometry), and chemical properties. It includes measurements from eight variants, considering four tree species and two land preparation methods for regeneration: with and without charcoal removal. The methodology and study location are described in the publication.
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Ziegler, Nancy, Nicholas Webb, Adrian Chappell, and Sandra LeGrand. Scale invariance of albedo-based wind friction velocity. Engineer Research and Development Center (U.S.), 2021. http://dx.doi.org/10.21079/11681/40499.

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Obtaining reliable estimates of aerodynamic roughness is necessary to interpret and accurately predict aeolian sediment transport dynamics. However, inherent uncertainties in field measurements and models of surface aerodynamic properties continue to undermine aeolian research, monitoring, and dust modeling. A new relation between aerodynamic shelter and land surface shadow has been established at the wind tunnel scale, enabling the potential for estimates of wind erosion and dust emission to be obtained across scales from albedo data. Here, we compare estimates of wind friction velocity (u*)
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Shani, Uri, Lynn Dudley, Alon Ben-Gal, Menachem Moshelion, and Yajun Wu. Root Conductance, Root-soil Interface Water Potential, Water and Ion Channel Function, and Tissue Expression Profile as Affected by Environmental Conditions. United States Department of Agriculture, 2007. http://dx.doi.org/10.32747/2007.7592119.bard.

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Constraints on water resources and the environment necessitate more efficient use of water. The key to efficient management is an understanding of the physical and physiological processes occurring in the soil-root hydraulic continuum.While both soil and plant leaf water potentials are well understood, modeled and measured, the root-soil interface where actual uptake processes occur has not been sufficiently studied. The water potential at the root-soil interface (yᵣₒₒₜ), determined by environmental conditions and by soil and plant hydraulic properties, serves as a boundary value in soil and p
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Савосько, Василь Миколайович, Юлія Бєлик, and Юрій Васильович Лихолат. Ecological and Geological Determination of the Initial Pedogenesis on Devastated Lands in the Kryvyi Rih Iron Mining & Metallurgical District (Ukraine). Journ. Geol. Geograph. Geoecology, 2019. http://dx.doi.org/10.31812/123456789/3643.

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In our time, a very urgent problem is the cessation of negative impacts on the environment and the return to the practical use of the territories of devastated lands. In this regard, it is important to find out the basic laws of primary soil formation in the area of these man-made neoplasms. The initial soil formation conditions were analyzed on 19 experimental sites which represent the main varieties of devastated land in the Kryvyi Rih Iron Mining and Metallurgical District (Central Ukraine): (i) waste rock dumps of old iron mines (old name “Forges”), (ii) tailing storage facility of undergr
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Christensen, Steen. Documentation of Edcrop – version 1: A Python package to simulate field-scale evapotranspiration and drainage from crop, wetland, or forest. Royal Danish Library, 2024. http://dx.doi.org/10.7146/aul.539.

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Evapotranspiration is one of the major components of Earth’s Water Balance, being the sum of evaporation and plant transpiration from the land and ocean surface. This report documents edcrop, a Python package that use climate input to simulate field-scale evapotranspiration and drainage from the root zone of an area covered with a crop, a wetland, or a forest. The conceptual model implemented in edcrop is a modification of the Evacrop model by Olesen and Heidmann (2002), which itself builds on the Watcros model by Aslyng and Hansen (1982). The edcrop conceptualization is based on consideration
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Baker, Christopher, Amanda Barker, Thomas Douglas, Stacey Doherty, and Robyn Barbato. Seasonal variation in near-surface seasonally thawed active layer and permafrost soil microbial communities. Engineer Research and Development Center (U.S.), 2024. http://dx.doi.org/10.21079/11681/48754.

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Understanding how soil microbes respond to permafrost thaw is critical to predicting the implications of climate change for soil processes. However, our knowledge of microbial responses to warming is mainly based on laboratory thaw experiments, and field sampling in warmer months when sites are more accessible. In this study, we sampled a depth profile through seasonally thawed active layer and permafrost in the Imnavait Creek Watershed, Alaska, USA over the growing season from summer to late fall. Amplicon sequencing showed that bacterial and fungal communities differed in composition across
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