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Journal articles on the topic 'Soil processes'

Author: Grafiati

Published: 4 June 2021

Last updated: 25 July 2025

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1

Pukish, Arsen, Yaroslav Adamenko, and Mirela Coman. "PEDOLOGICAL PROCESSES IN TECHNOSOILS." Scientific Bulletin Series D : Mining, Mineral Processing, Non-Ferrous Metallurgy, Geology and Environmental Engineering 32, no. 1 (2018): 73–79. http://dx.doi.org/10.37193/sbsd.2018.1.10.

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The article studies the correlation and regression analysis concentration of main ions in the soil. According to the research the empirical equations was received. The obtained dependencies can be used in the analytical studies of soil samples, modeling of salts dissemination in the soil, development of measures for the soil restoration, calculation of the needed amounts of subsidiary chemicals for saline soils restoration.

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2

Poyon Kizi, Khayitova Sanobar. "SOIL SCIENCE AND SOIL TERMINOLOGY." European International Journal of Multidisciplinary Research and Management Studies 02, no. 11 (2022): 42–44. http://dx.doi.org/10.55640/eijmrms-02-11-12.

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Soil science involves the study of the formation and distribution of soil, the biological, chemical and physical properties and processes of soil and how these processes interact with wider systems to help inform environmental management, industry and sustainable development.

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3

Gadjalska, Nelly, Rossitza Petrova, Snejan Bozhkov, and Viktoriya Kancheva. "Erosion Processes Due to Sprinkler Irrigation." Bulgarian Journal of Soil Science 6, no. 1 (2021): 59–64. https://doi.org/10.5281/zenodo.4887457.

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The study and analyses of erosion have shown that the main factors determining erosion processes under equal soil and climatic conditions are the intensity and structure of artificial rain and the ground slope. The main factor, artificial rain intensity, depends mainly on the soil infiltration rate. In sprinkle irrigation, the soil infiltration is preceded by interaction between the soil and the rainfall drops. Failure to observe this interaction has often caused irrigation erosion problems due to the impact drops on the soil. It has been proved that the bigger are rainfall drops and their int

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Andronov, E. E., E. A. Ivanova, E. V. Pershina, et al. "Analysis of soil microbiome indicators in processes of soil formation, organic matter transformation and processes involved with fine regulation of vegetative processes." Dokuchaev Soil Bulletin, no. 80 (September 1, 2015): 83–94. http://dx.doi.org/10.19047/0136-1694-2015-80-83-94.

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At the current stage of soil microbiology development the study of the entire complex of microorganisms inhabiting the soil became possible, which helps finding the optimal combination of factors resulting in the formation of soil fertility as well as the development of stable and stress resistant phytocenosis. Soil metagenome is the largest genetic depository for all purposes, from the soil formation processes - transformation of barren rock into a substrate for plant growth and development, to the temporary adaptations in the short-term interests of the plant. The investigation of genetic po

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Savich, Vitaliy, Vladimir Sedykh, and Nikolay Minaev. "Information assessment of the interrelationships of soil properties, processes and regimes." АгроЭкоИнфо 6, no. 54 (2022): 42. http://dx.doi.org/10.51419/202126642.

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The interrelationships of soil properties, processes and regimes occurring in them characterize the genesis, agroecological state and fertility of soils. The use of organic and mineral fertilizers changes the properties of soils and the relationship between soil properties. The effect of the introduction of siderates and NPK into the soil on the enzymatic and microbiological activity of soils is shown. Data on changes in the fractional composition of iron in different horizons of podzolic soil are presented. It is proved that the relationship between soil properties is one of the factors deter

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Komiljon Ogli, Nurullaev Azamkhon, and Djalilova Gulnora Tulkunovna. "EFFECT OF EROSION PROCESSES ON SOIL PROPERTIES." American Journal Of Agriculture And Horticulture Innovations 3, no. 12 (2023): 5–12. http://dx.doi.org/10.37547/ajahi/volume03issue12-02.

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Today, global climate change, along with drought, the processes of soil degradation are becoming one of the urgent problems for scientists all over the world. In this regard, a number of works are being carried out in Uzbekistan. According to the National Report on the State of Land Resources of the Republic of Uzbekistan, only 10% (4.3 million ha) of the 44.9 million hectares in the Republic are irrigated. About 2 million hectares (45%) of these lands are subject to secondary salinization. There are problems with water erosion on 800,000 hectares and wind erosion on 2 million hectares. The ob

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Baldrian, P. "Microbial enzyme-catalyzed processes in soils and their analysis." Plant, Soil and Environment 55, No. 9 (2009): 370–78. http://dx.doi.org/10.17221/134/2009-pse.

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Currently, measuring enzyme activities in soils or other lignocellulose-based materials is technically feasible; this measurement is particularly suitable for evaluating soil processes of biopolymer (cellulose, hemicelluloses, lignin, chitin and others) degradation by microbes and for assessing cycling and mobilization of principal nutrients including nitrogen, phosphorus and sulfur. With some considerations, assay methods can provide reliable information on the concentration of enzymes in soil or the rates of enzyme-catalyzed processes. Enzyme analyses in recent studies demonstrated a high le

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8

Beylich, Anneke, Hans-Rudolf Oberholzer, Stefan Schrader, Heinrich Höper, and Berndt-Michael Wilke. "Evaluation of soil compaction effects on soil biota and soil biological processes in soils." Soil and Tillage Research 109, no. 2 (2010): 133–43. http://dx.doi.org/10.1016/j.still.2010.05.010.

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9

Stonehouse, Bernard. "Biological processes in cold soils." Polar Record 35, no. 192 (1999): 5–10. http://dx.doi.org/10.1017/s0032247400026279.

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AbstractThis paper presents a simple model of processes by which soils develop in polar and high-altitude regions. It reviews influences of seasonal freezing, permafrost, and vegetation on soil formation; discusses recently formulated concepts of disturbance and damage; and draws attention to developments in remediation, especially possibilities for encouraging natural soil regeneration and rehabilitation processes.

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10

Nagare, R. M., P. Bhattacharya, J. Khanna, and R. A. Schincariol. "Coupled cellular automata for frozen soil processes." SOIL Discussions 1, no. 1 (2014): 119–50. http://dx.doi.org/10.5194/soild-1-119-2014.

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Abstract. Heat and water movement in variably saturated freezing soils is a tightly coupled phenomenon. Strong coupling of water and heat movement in frozen soils moves considerable amounts of water from warmer to colder zones. The coupling is a result of effects of sub-zero temperature on soil water potential, heat carried by water moving under pressure gradients, and dependency of soil thermal and hydraulic properties on soil water content. This makes water and heat movement in variably saturated soils a highly non-linear process in mathematical terms. This study presents a one-dimensional c

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Lemega, Nadiya. "Degradation processes in the soils of the Kolodnytsia River basin." Visnyk of the Lviv University. Series Geography, no. 51 (December 27, 2017): 193–203. http://dx.doi.org/10.30970/vgg.2017.51.8858.

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This article presents the results of soil degradation studies of the Kolodnytsia River basin. The basin approach is applied in soil-geographical studies. The conditions for the formation of soils are studied depending on the morphometric characteristics of the river basin and soil-bearing rocks. The analysis of the causes of the spread of degradation processes of various species, which cause soil degradation, is carried out. Particular attention is paid to the anthropogenic factor of soil degradation, which began with the development of the territory by white Croats, that is, more than a thous

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Sultanov, Karim, Pavel Loginov, Sabida Ismoilova, and Zulfiya Salikhova. "Wave processes in determining mechanical characteristics of soils." E3S Web of Conferences 97 (2019): 04009. http://dx.doi.org/10.1051/e3sconf/20199704009.

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Mechanical characteristics of soils under dynamic and static loads are determined in laboratory conditions on special devices. Dynamic loads in the devices are initiated by an impact on a soil sample. Under the impact the waves are initiated in soil; they significantly affect the stress-strain state of soil samples placed in the device. Depending on the parameters of the impact load in the device, in different sections of soil sample there arise the stress-strain states, different in quality and quantity. Mechanical characteristics of soil, determined by this stress-strain state, also differ.

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Podvolotskaya, Guriyat, Sergey Belopukhov, Vitaly Savich, Andrey Sorokin, and Nikolay Tyutrin. "Properties, processes and regimes of soil solutions and surface waters." E3S Web of Conferences 175 (2020): 12022. http://dx.doi.org/10.1051/e3sconf/202017512022.

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Soil solutions and the surface waters are characterized by properties, processes and regimes. Soil solutions of different soils and their surface water have different biological activity and change the activity of dissolved stimulants and inhibitors. The object of the study are soil solutions of the main types of soils obtained in the model experiments with the ratio of soils: water equal to 1:1 and 1: 2, soil solutions and surface water in the flooding of soils with water for 1 week – 3 months. The research method consisted in the assessment of pH, Eh, activity of K, NO3, NH4, Ca, Mg by conve

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Nagare, R. M., P. Bhattacharya, J. Khanna, and R. A. Schincariol. "Coupled cellular automata for frozen soil processes." SOIL 1, no. 1 (2015): 103–16. http://dx.doi.org/10.5194/soil-1-103-2015.

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Abstract. Heat and water movement in variably saturated freezing soils is a strongly coupled phenomenon. The coupling is a result of the effects of sub-zero temperature on soil water potential, heat carried by water moving under pressure gradients, and dependency of soil thermal and hydraulic properties on soil water content. This study presents a one-dimensional cellular automata (direct solving) model to simulate coupled heat and water transport with phase change in variably saturated soils. The model is based on first-order mass and energy conservation principles. The water and energy fluxe

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15

Huang, Mingbin, S. Lee Barbour, Amin Elshorbagy, Julie D. Zettl, and Bing Cheng Si. "Infiltration and drainage processes in multi-layered coarse soils." Canadian Journal of Soil Science 91, no. 2 (2011): 169–83. http://dx.doi.org/10.4141/cjss09118.

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Huang, M., Barbour, S. L., Elshorbagy, A., Zettl, J. D. and Si, B. C. 2011. Infiltration and drainage processes in multi-layered coarse soils. Can. J. Soil Sci. 91: 169–183. Infiltration and drainage processes in multi-layered soils are complicated by contrasting hydraulic properties. The objective of this study was to evaluate the performances of the hysteretic and non-hysteretic models to simulate the infiltration and drainage processes from three different natural soil profiles containing as many as 20 texturally different layers. Hydraulic properties were estimated from soil textures using

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16

Jimenez, Laís Coutinho Zayas, Hermano Melo Queiroz, Gabriel Nuto Nóbrega, et al. "Recovery of Soil Processes in Replanted Mangroves: Implications for Soil Functions." Forests 13, no. 3 (2022): 422. http://dx.doi.org/10.3390/f13030422.

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Mangrove revegetation is a vital strategy to recover ecosystem services (e.g., climate regulation and pollutants retention) provided by these ecosystems. Although soils are directly or indirectly responsible for diverse ecosystem services in mangrove ecosystems, few studies have focused on the recovery of soil functions (e.g., carbon sequestration) after mangrove replanting. This study aimed to evaluate the recovery of soil processes associated with Fe, S, and C dynamics and its implications for the restoration of soil functions. Two mangrove sites under replanting initiatives were studied alo

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Zaitsev, Y., V. Sobko, V. Kozhevnikova, О. Lobanova, and A. Kyrylchuk. "Classification of processes that cause land degradation." Agroecological journal, no. 3 (September 6, 2022): 150–59. http://dx.doi.org/10.33730/2077-4893.3.2022.266420.

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It is highlighted that the current state of agricultural landscapes is characterized by a significant increase in the area of eroded arable land, which amounts to about 11 million hectares, and eroded agricultural lands — more than 13 million hectares (32.0% of their total area). Modern land-tenancy relations do not contribute to the implementation of measures to protect and increase soil fertility and have a negative effect on their fertility. In the process of using the soil cover, the needs and requirements of the ecobalance are ignored, as a result of which agricultural land is exhaustingl

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Rengasamy, Pichu. "Soil processes affecting crop production in salt-affected soils." Functional Plant Biology 37, no. 7 (2010): 613. http://dx.doi.org/10.1071/fp09249.

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Salts can be deposited in the soil from wind and rain, as well as through the weathering of rocks. These processes, combined with the influence of climatic and landscape features and the effects of human activities, determine where salt accumulates in the landscape. When the accumulated salt in soil layers is above a level that adversely affects crop production, choosing salt-tolerant crops and managing soil salinity are important strategies to boost agricultural economy. Worldwide, more than 800 million hectares of soils are salt-affected, with a range of soils defined as saline, acidic–salin

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19

Vogelmann, Eduardo Saldanha, José Miguel Reichert, Juliana Prevedello, and Gabriel Oladele Awe. "Hydro-physical processes and soil properties correlated with origin of soil hydrophobicity." Ciência Rural 43, no. 9 (2013): 1582–89. http://dx.doi.org/10.1590/s0103-84782013005000107.

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Hydrophobicity is the phenomenon where the soil has reduced wettability, usually associated with coating of soil particles by hydrophobic organic substances. This study aimed to provide a description of the hydrophobicity occurrence, highlight recent discoveries about the origin of phenomenon and discuss the main hydro-physical properties and chemical processes linked to the development of hydrophobic behavior in soils. Hydrophobicity is associated with other factors such as soil moisture, presence of some fungi species, particle size, soil pH and occurrence of burnings. The causative substanc

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20

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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de Jonge, L. W., P. Moldrup, and P. Schjønning. "Soil Infrastructure, Interfaces and Translocation Processes in Inner Space (''Soil-it-is''): towards a road map for the constraints and crossroads of soil architecture and biophysical processes." Hydrology and Earth System Sciences Discussions 6, no. 2 (2009): 2633–78. http://dx.doi.org/10.5194/hessd-6-2633-2009.

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Abstract. Soil functions and their impact on health, economy and the environment are evident at the macro scale but determined at the micro scale, based on interactions between soil micro-architecture and the transport and transformation processes occurring in the pore and particle networks and at their interfaces. Soil structure formation and its resilience to disturbance are highly dynamic features affected by management (energy input), moisture (matric potential), and solids composition and complexation (organic carbon, OC, and clay interactions). In this paper we review and put into perspe

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22

Barbosa Ferreira, Maiara, Aline Maria Sales Solano, Elisama Vieira dos Santos, Carlos A. Martínez-Huitle, and Soliu O. Ganiyu. "Coupling of Anodic Oxidation and Soil Remediation Processes: A Review." Materials 13, no. 19 (2020): 4309. http://dx.doi.org/10.3390/ma13194309.

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In recent years, due to industrial modernization and agricultural mechanization, several environmental consequences have been observed, which make sustainable development difficult. Soil, as an important component of ecosystem and a key resource for the survival of human and animals, has been under constant contamination from different human activities. Contaminated soils and sites require remediation not only because of the hazardous threat it possess to the environment but also due to the shortage of fresh land for both agriculture and urbanization. Combined or coupled remediation technologi

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Taraqqi-A-Kamal, A., Christopher J. Atkinson, Aimal Khan, et al. "Biochar remediation of soil: linking biochar production with function in heavy metal contaminated soils." Plant, Soil and Environment 67, No. 4 (2021): 183–201. http://dx.doi.org/10.17221/544/2020-pse.

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The focus of this study is on the soil physicochemical, biological, and microbiological processes altered by biochar application to heavy metal (HM) contaminated soils. The aim is to highlight agronomical and environmental issues by which the restorative capacity of biochar might be developed. Literature shows biochar can induce soil remediation, however, it is unclear how soil processes are linked mechanistically to biochar production and if these processes can be manipulated to enhance soil remediation. The literature often fails to contribute to an improved understanding of the mechanisms b

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Maier, Martin, Valentin Gartiser, Alexander Schengel, and Verena Lang. "Long Term Soil Gas Monitoring as Tool to Understand Soil Processes." Applied Sciences 10, no. 23 (2020): 8653. http://dx.doi.org/10.3390/app10238653.

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Soils provide many functions as they represent a habitat for flora and fauna, supply water, nutrient, and anchorage for plant growth and more. They can also be considered as large bioreactors in which many processes occur that involve the consumption and production of different gas species. Soils can be a source and sink for greenhouse gases. During the last decades this topic attracted special attention. Most studies on soil-atmosphere gas fluxes used chamber methods or micro-meteorological methods. Soil gas fluxes can also be calculated from vertical soil gas profiles which can provide addit

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Kobza, Jozef, Gabriela Barančíková, Jarmila Makovníková, Boris Pálka, Ján Styk, and Miloš Širáň. "Current State and Development of Land Degradation Processes Based on Soil Monitoring in Slovakia." Agriculture (Pol'nohospodárstvo) 63, no. 2 (2017): 74–85. http://dx.doi.org/10.1515/agri-2017-0007.

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Abstract Current state and development of land degradation processes based on soil monitoring system in Slovakia is evaluated in this contribution. Soil monitoring system in Slovakia is consistently running since 1993 year in 5-years repetitions. Soil monitoring network in Slovakia is constructed using ecological principle, taking into account all main soil types and subtypes, soil organic matter, climatic regions, emission regions, polluted and non-polluted regions as well as various land use. The result of soil monitoring network is 318 sites on agricultural land in Slovakia. Soil properties

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Liu, Q., P. Loganathan, M. J. Hedley, and M. F. Skinner. "Root processes influencing phosphorus availability in volcanic soils under young Pinus radiata plantations." Canadian Journal of Forest Research 36, no. 8 (2006): 1913–20. http://dx.doi.org/10.1139/x06-083.

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Phosphorus (P) availability was investigated in rhizosphere soils under 4- to 5-year-old, second-rotation Pinus radiata D. Don and understorey grass (browntop, Agrostis capillaris L.) in two P-deficient Andosols (a Pumice Soil and an Allophanic Soil). Pinus radiata rhizosphere had more soil organic matter, greater mycorrhizal hyphal length density, higher acid phosphatase activity, and more concentrated dissolved organic carbon than bulk soil or the rhizosphere of grass species in one or both soils. Concentrations of resin P and organic P in the P. radiata rhizosphere were higher than those in

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Lipkovich, Igor, Irina Egorova, Nadezhda Petrenko, Sai-Suu Saaya, Dinara Zalyakaeva, and Stanislav Akhmetshin. "Greening of processes in soil cultivation." BIO Web of Conferences 105 (2024): 01001. http://dx.doi.org/10.1051/bioconf/202410501001.

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The article analyzes the factors affecting the soil, which directly affect the yield. Modern domestic agricultural machinery mainly has technical and technological solutions that make it possible to significantly advance in the direction of ecological balance of the impact of crop production on soils. These include non-fallow, combined techniques of basic and pre-sowing tillage, as well as the use of a new complex of heavy agrophilic running systems of heavy mobile power facilities.

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Reinsch, Sabine, David A. Robinson, Maud A. J. van Soest, Aidan M. Keith, Simon Parry, and Andrew M. Tye. "Temperate Soils Exposed to Drought—Key Processes, Impacts, Indicators, and Unknowns." Land 13, no. 11 (2024): 1759. http://dx.doi.org/10.3390/land13111759.

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The summer drought in the United Kingdom (UK) in 2022 produced significant speculation concerning how its termination may impact and interact with the soil resource. Whilst knowledge regarding soils and droughts exists in the scientific literature, a coherent understanding of the wider range of impacts on soil properties and functions has not been compiled for temperate soils. Here, we draw together knowledge from studies in the UK and other temperate countries to understand how soils respond to drought, and importantly what and where our knowledge gaps are. First, we define the different type

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de Jonge, L. W., P. Moldrup, and P. Schjønning. "Soil Infrastructure, Interfaces & Translocation Processes in Inner Space ("Soil-it-is"): towards a road map for the constraints and crossroads of soil architecture and biophysical processes." Hydrology and Earth System Sciences 13, no. 8 (2009): 1485–502. http://dx.doi.org/10.5194/hess-13-1485-2009.

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Abstract. Soil functions and their impact on health, economy, and the environment are evident at the macro scale but determined at the micro scale, based on interactions between soil micro-architecture and the transport and transformation processes occurring in the soil infrastructure comprising pore and particle networks and at their interfaces. Soil structure formation and its resilience to disturbance are highly dynamic features affected by management (energy input), moisture (matric potential), and solids composition and complexation (organic matter and clay interactions). In this paper we

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Shao, Yaping, Klaus Fraedrich, and Masahide Ishizuka. "Modelling Soil Moisture in Hyper-Arid Conditions." Boundary-Layer Meteorology 179, no. 2 (2021): 169–86. http://dx.doi.org/10.1007/s10546-020-00596-9.

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AbstractIn most land-surface models, the evolution of soil moisture is governed by soil-hydraulic processes. In hyper-arid soils, these processes break down, but soil moisture continues to show clear temporal variations, suggesting that other processes may be at work. We hypothesize that moisture in such soils varies due to evaporation in the soil and to vapour fluxes at the air–soil interface. To test this, we include vapour exchange between the air and soil in a land-surface model, apply the model to a desert site, and compare the simulated and observed soil moisture. The good agreement betw

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Gasimov, L. "Degradation processes in the Lankaran Lowland soils of Azerbaijan Republic." Bulletin of Science and Practice 5, no. 1 (2019): 172–76. https://doi.org/10.5281/zenodo.2539643.

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The article presents an analysis of archival materials and their own research to assess the intensive development of soil degradation of the Lenkoran lowland of the Republic of Azerbaijan as a result of the influence of climatic and anthropogenic factors. The degradation processes of one soil-plant nomenclature of taxa to another are revealed. This is due to increased anthropogenic influences and climate warming processes. In the northern half of the subarea under study, yellow earth soils were deformed to yellow earth meadow soils. In the upper layers of the profile of yellow–gley

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Elzinga, Evert J., and Yuji Arai. "Sorption Processes in Soils and Sediments." Soil Systems 5, no. 4 (2021): 70. http://dx.doi.org/10.3390/soilsystems5040070.

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Sorption processes at the mineral–water interface are fundamental to the chemical functioning of soils, and impact the biogeochemical cycling of both trace and major elements in soil and sediment environments [...]

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Gelfan, А. N. "Assessing predictability of hydrological processes (on the example of frozen soil water content dynamics)." Гидросфера. Опасные процессы и явления 4, no. 2 (2020): 365–74. http://dx.doi.org/10.34753/hs.2020.2.4.365.

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A method has been developed for assessing the limits of predictability of the frozen soil water content (according to observations at the Nizhnedevitskaya water balance station). The method is based on the analysis of the convergence of a given probabilistic measure (the variance of the calculated soil water content at a given date) to its stable value. The soil water content was simulated by the physically based model of heat and water transfer in a frozen soil column during a autumn-winter seasons. To assess variability of the modelled soil water content at a given date, the boundary meteoro

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Tsoraeva, Eleonora, Larisa Basieva, and Batrbek Kozyrev. "The impact of the development of negative soil processes on the land fund of the Russian Federation." BIO Web of Conferences 43 (2022): 02005. http://dx.doi.org/10.1051/bioconf/20224302005.

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One of the reasons of the reduction of agricultural land is the degradation of soil processes. The main negative processes occurring in soils and leading to their degradation are erosion (water and wind), reduction of humus content in the soil. A significant spread of negative processes developing due to the action of natural and anthropogenic factors leads to a critical decrease in soil fertility. By washing away the upper fertile soil layer and the formation of large gullies due to improper tillage, soil erosion is formed. In order to prevent soil erosion, it is necessary to take measures to

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Brevik, Eric C. "Soils and Climate Change: Gas Fluxes and Soil Processes." Soil Horizons 53, no. 4 (2012): 12. http://dx.doi.org/10.2136/sh12-04-0012.

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Kuhlman, M. I., and T. M. Greenfield. "Simplified soil washing processes for a variety of soils." Journal of Hazardous Materials 66, no. 1-2 (1999): 31–45. http://dx.doi.org/10.1016/s0304-3894(98)00212-x.

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Peth, S., J. Rostek, A. Zink, A. Mordhorst, and R. Horn. "Soil testing of dynamic deformation processes of arable soils." Soil and Tillage Research 106, no. 2 (2010): 317–28. http://dx.doi.org/10.1016/j.still.2009.10.007.

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Lingineni, Suresh, and Vijay K. Dhir. "Modeling of Soil Venting Processes to Remediate Unsaturated Soils." Journal of Environmental Engineering 118, no. 1 (1992): 135–52. http://dx.doi.org/10.1061/(asce)0733-9372(1992)118:1(135).

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39

Breemen, N. van. "Effects of redox processes on soil acidity." Netherlands Journal of Agricultural Science 35, no. 3 (1987): 271–79. http://dx.doi.org/10.18174/njas.v35i3.16724.

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Redox processes due to alternating aerobic and anaerobic conditions may give rise to strongly acidic or alkaline soils and waters. First, oxidized chemical components tend to be more acidic or less alkaline than their reduced counterparts. Second, and more important, redox processes often lead to the simultaneous formation of acidic (or potentially acidic) and alkaline substances with different mobility (dissolved or gaseous versus adsorbed or solid), so that one of the two substances can be exported, leaving a more acidic or more alkaline residue. Examples of acidification or alkalinization p

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Morgunov, K. P., M. A. Kolosov, and P. P. Chinakov. "Using liquefaction and consolidation processes to control soil properties." Vestnik Gosudarstvennogo universiteta morskogo i rechnogo flota imeni admirala S. O. Makarova 17, no. 1 (2025): 21–32. https://doi.org/10.21821/2309-5180-2025-17-1-21-32.

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An analysis of the impact of water from streams and reservoirs on the banks of reservoirs and soil massifs of artificial embankments – dams, dikes, and embankments – was carried out. It has been determined that the main factor influencing the condition of banks and embankment soils is their saturation with water and the formation of filtration flows in soil massifs, sometimes with quite significant gradients. The main processes that determine the state of structures are the processes of loosening and liquefaction of soils and their subsequent consolidation. The processing of reservoir banks co

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Guicharnaud, R., O. Arnalds, and G. I. Paton. "Short term changes of microbial processes in Icelandic soils to increasing temperatures." Biogeosciences 7, no. 2 (2010): 671–82. http://dx.doi.org/10.5194/bg-7-671-2010.

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Abstract. Temperature change is acknowledged to have a significant effect on soil biological processes and the corresponding sequestration of carbon and cycling of nutrients. Soils at high latitudes are likely to be particularly impacted by increases in temperature. Icelandic soils experience unusually frequent freeze and thaw cycles compare to other Arctic regions, which are increasing due to a warming climate. As a consequence these soils are frequently affected by short term temperature fluctuations. In this study, the short term response of a range of soil microbial parameters (respiration

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Quideau, S. A., M. J. B. Swallow, C. E. Prescott, S. J. Grayston, and S. W. Oh. "Comparing soil biogeochemical processes in novel and natural boreal forest ecosystems." Biogeosciences 10, no. 8 (2013): 5651–61. http://dx.doi.org/10.5194/bg-10-5651-2013.

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Abstract. Emulating the variability that exists in the natural landscape prior to disturbance should be a goal of soil reconstruction and land reclamation efforts following resource extraction. Long-term ecosystem sustainability within reclaimed landscapes can only be achieved with the re-establishment of biogeochemical processes between reconstructed soils and plants. In this study, we assessed key soil biogeochemical attributes (nutrient availability, organic matter composition, and microbial communities) in reconstructed, novel, anthropogenic ecosystems, covering different reclamation treat

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Quideau, S. A., M. J. B. Swallow, C. E. Prescott, S. J. Grayston, and S. W. Oh. "Comparing soil biogeochemical processes in novel and natural boreal forest ecosystems." Biogeosciences Discussions 10, no. 4 (2013): 7521–48. http://dx.doi.org/10.5194/bgd-10-7521-2013.

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Abstract. Emulating the variability that exists in the natural landscape prior to disturbance should be a goal of soil reconstruction and land reclamation efforts following resource extraction. Long-term ecosystem sustainability within reclaimed landscapes can only be achieved with the re-establishment of biogeochemical processes between reconstructed soils and plants. In this study, we assessed key soil biogeochemical attributes (nutrient availability, organic matter composition, and microbial communities) in reconstructed, novel, anthropogenic ecosystems covering different reclamation treatm

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Sorokin, Andrey, Sergey Belopukhov, Vladimir Gukalov, Vitaly Savich, Ravil Baibekov, and Nikolay Tyutrin. "Properties, processes and modes characterizing the state of heavy metals in soils." E3S Web of Conferences 285 (2021): 06007. http://dx.doi.org/10.1051/e3sconf/202128506007.

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The study proves the expediency of assessing the state of heavy metals in soils by the fractional composition of soil compounds, processes and modes. An informational and energy analysis of the state of heavy metals in soils was carried out. The need for an assessment of the kinetics of their desorption from soils was substantiated. The CH3 COONH4 solution displaced 0.3 mg/l Mn from the sod-podzolic soil within 10 minutes, 0.8 mg/l Mn – within 1 hour, 3.3 mg/l Mn – within 1 day, and 12.9 mg/l – within one week; 0.18 mg/L Pb was desorbed within 10 minutes, up to 0.59 mg/l Pb was desorbed within

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Park, So Yun, Jae Gyeong Kim, and Eun Hea Jho. "Degradation of Oxolinic Acid in Soil Under Simulated Natural Degradation Processes." Journal of Korean Society of Environmental Engineers 47, no. 1 (2025): 1–12. https://doi.org/10.4491/ksee.2025.47.1.1.

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Oxolinic acid (OA), a quinolone-class antibiotic commonly used in domestic agriculture, exhibits low bioavailability, raising concerns about its potential environmental persistence. Residual OA in the environment can undergo partial degradation through natural processes, which are influenced by various factors. This study aimed to investigate the photodegradation and biodegradation patterns of OA under various environmental factors, including temperature, light intensity, soil usage, soil organic matter content (OM). Additionally, adsorption and desorption experiments were conducted to elucida

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Vasu, Duraisamy, Surendra Kumar Singh, Pramod Tiwary, Padikkal Chandran, Sanjay Kumar Ray, and Veppangadu Perumal Duraisami. "Pedogenic processes and soil–landform relationships for identification of yield-limiting soil properties." Soil Research 55, no. 3 (2017): 273. http://dx.doi.org/10.1071/sr16111.

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Knowledge of soil–landform relationships helps in understanding the dominant pedogenic processes causing variations in soil properties within and between landforms. In this study, we investigated how major pedogenic processes in three landform positions of the semi-arid Deccan Plateau (India) have led to current plant yield-limiting soil properties. For this, we characterised 26 pedons from three landforms – piedmont, alluvial plain and valley – and performed factor analysis on the dataset. As the frequency distribution of the dataset was highly skewed for most of the soil properties, landform

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Wild, A., and S. Ross. "Soil Processes: A Systematic Approach." Journal of Applied Ecology 27, no. 1 (1990): 361. http://dx.doi.org/10.2307/2403600.

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Popov, Leonid, Gheorghe Ciudin, and Serghei Rotaru. "Soil Degradation Processes from Pollution." Chemistry Journal of Moldova 7, no. 1 (2012): 50–53. http://dx.doi.org/10.19261/cjm.2012.07(1).07.

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Investigations found HCH and DDT residuals in bottom sediments from several reservoirs and lakes as well as the main rivers, Nistru and Prut (concentrations ranged between 0.2 and 15.8 ppb). The concentration of PCBs in the topsoil collected beneath the capacitors battery at the Vulcănesti substation reached a level of 7100 ppm which is exceeding the MAC by five orders of magnitude (!). With no exception, allowable concentrations of PCBs in soil were exceeded also on the territory of other investigated substations, with peaks registered at the Briceni substation (2545 ppm) and the Orhei substa

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Selim, H. M. "Soil Pollution: Processes and Dynamics." Soil Science 162, no. 12 (1997): 953–54. http://dx.doi.org/10.1097/00010694-199712000-00010.

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Loveland, P. "Soil pollution. Processes and dynamics." Geoderma 75, no. 1-2 (1997): 150–52. http://dx.doi.org/10.1016/s0016-7061(96)00082-1.

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