Academic literature on the topic 'Typical gray soils'

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Journal articles on the topic "Typical gray soils"

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Burkhanova, D., and M. Urmanova. "Morphological structure, agrophysical and agrochemical properties of irrigated typical gray and grass soils." E3S Web of Conferences 371 (2023): 01020. http://dx.doi.org/10.1051/e3sconf/202337101020.

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The article presents information on morphological structures, general physical and agrochemical properties of typical irrigated gray and grassland soils. The general physical properties of the soil are that in typical gray soils the bulk density decreases and the porosity increases, while in grassland soils the bulk density decreases and the total porosity increases compared to typical gray soils. A typical irrigated gray soil is composed of large dust particles according to its mechanical composition and belongs to the category of medium sandy loam. According to the level of availability of humus and nutrients of the studied soils, typical gray and meadow soils irrigated are low in humus (0.36-0.87%), very low in mobile phosphorus (5.33-15.60 mg/kg), exchangeable potassium It is highlighted that it is provided with low (100-200 mg/kg).
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Burkhanova, Dilnavoza, Dilrabo Kodirova, Munisa Urmanova, Muradjan Karimov, and Matlyuba Usmonova. "Perceived methods for increasing the productivity of irrigated typical gray and grazing soils of Uzbekistan in non-traditional irrigation." E3S Web of Conferences 258 (2021): 03024. http://dx.doi.org/10.1051/e3sconf/202125803024.

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This article considers the effective effect of mulching of irrigated typical gray and meadow soils with plant residues and application of various fertilizers on soil fertility, mulching of typical gray soils with plant residues and application of various fertilizers (organic fertilizers, biohumus and biopreparations) in meadow soils. The effect on microbiological activity was determined. The application of various fertilizers (organic fertilizers, biohumus and biopreparations) to typical irrigated gray and meadow soils and mulching of the soil with plant residues have been shown to affect the growth and yield of winter wheat and cotton.
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Burkhanova, Dilnavoza, Munisa Urmanova, and Gulchekhra Sodikova. "Morphological structures and properties of typical irrigated gray soils: A case study of Tashkent province." E3S Web of Conferences 563 (2024): 03030. http://dx.doi.org/10.1051/e3sconf/202456303030.

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The research detailed in the article offers a comprehensive examination of typical irrigated gray soils, focusing on their morphological features and fundamental physical and agrochemical characteristics. A critical observation from the study is the variation in bulk density and porosity among these soils. Specifically, it was noted that in typical gray soils, there is a marked decrease in bulk density coupled with an increase in porosity, suggesting a structure that, while dense, allows for significant air and water movement within the soil matrix. The mechanical composition of these soils is primarily characterized by large dust particles and a texture classified as heavy sand. This specific composition impacts both the soil's water-holding capacity and its aeration, factors crucial for plant root development and microbial activity. From an agrochemical standpoint, the research underscores a variance in nutrient levels within typical irrigated gray soils. The humus content, a key indicator of soil fertility, was found to range from low to medium levels, with percentages between 0.35% and 1.13%. This range signifies a modest capability of the soil to sustain plant life, impacting agricultural productivity and necessitating careful soil management practices to enhance organic matter content. The study highlights the nutrient availability in these soils, particularly pointing out the very low levels of mobile phosphorus (ranging from 4.0 to 13.46 mg/kg) and the low to moderate supply of exchangeable potassium (100-213 mg/kg).
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Gapparov, Islom Uchqun o'g'li Xolmo'minov Samandar Murodjon o'g'li Nodirova Nodira Jaxongir qizi Tirkashev Mirjahon Ulug'bek o'g'li. "AGROCHEMICAL AND BIOLOGICAL PROPERTIES OF IRRIGATED GRAY SOILS." INTERNATIONAL BULLETIN OF APPLIED SCIENCE AND TECHNOLOGY 3, no. 4 (2023): 994–1002. https://doi.org/10.5281/zenodo.7907841.

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The article provides information about the agrochemical properties and biological activity of typical irrigated serozem soils. The study of soil properties and biological activity is of great importance in increasing the fertility of typical irrigated serozem soils.
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Senicovscaia, Irina, Andrei Danilov, and Andriana Danilov. "BIODIVERSITY OF EDAPHIC FAUNA IN GRAY FOREST SOILS OF THE REPUBLIC OF MOLDOVA." Current Trends in Natural Sciences 10, no. 19 (2021): 134–41. http://dx.doi.org/10.47068/ctns.2021.v10i19.018.

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Gray forest soils of the natural ecosystems in the central and northern zones of the Republic of Moldova are the habitat and the source of conservation and reproduction of the edaphic fauna. They represent themselves the standards of the biodiversity for soil invertebrates. Invertebrates sampling was carried out from test cuts by manual sampling of soil layers to the depth of soil fauna occurrence. The main content of invertebrates in gray soils under the forest was in the layer of 0-20 cm. In addition to the Lumbricidae family there were found the species of the Clubionidae, Hydromiidae, Scarabaeidae, Oniscidae, Tortricidae, Julidae, Curculionidae, Carabidae, Geophilidae, Tenebrionidae, Melandryidae and Formicidae families. Species of Eisenia rosea, Euomphalia strigella, Formica rufa, Tortrix viridana, Curculio glandium, Melolontha melolontha and others have been identified in three subtypes of gray forest soils of natural ecosystems. The long use of these soils in agricultural production led to the considerable decrease in the number and biomass of invertebrates and degradation of the faunal complex in general. The number of families decreased from 6-12 to 1-3. Species of Lumbricidae, Elateridae, Tortricidae and Coccinellidae have been found in arable gray forest soils. The trophic pyramids are stable in the typical virgin gray soil. The relationship between trophic levels of the edaphic fauna in the typical gray forest soil is stronger in comparison with albic and molic gray forest soils.
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Эгамбердиев, Шердор Камилович Нематов Хуршид Мамадуллаевич Тоҳиров Алпомиш Одилбой ўғли. "EFFECT OF SIDERATES ON SOIL AGROCHEMICAL PROPERTIES." "Science and innovation" international scientific journal. ISSN: 2181-3337 1, no. 3 (2022): 122–28. https://doi.org/10.5281/zenodo.6678120.

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<em>The article describes the influence of green manure of agricultural crops on the amount of humus and mobile nutrients in the soil under the conditions of typical gray soils of the Samarkand region. According to the results obtained, the use of green peas and amaranth plants as green manures on typical irrigated gray soils has a positive effect on the amount of humus and mobile nutrients in the soil and increases their amount.</em>
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Gaffarova, Liliya. "DYNAMICS OF HUMUS RESERVES AND FORECAST OF CARBON-INVESTING POTENTIAL OF ZONAL SOILS OF THE REPUBLIC OF TATARSTAN." Vestnik of Kazan State Agrarian University 16, no. 3 (2021): 27–31. http://dx.doi.org/10.12737/2073-0462-2021-27-31.

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The article analyzes the results of statistical processing of morphometric and agrochemical indicators of zonal soils of the Republic of Tatarstan based on the accumulated information of large-scale soil studies. The boundaries of genetic horizons are examined, the content of humus and its reserves within the limits of heavy loamy and clay varieties of arable soil subtypes is estimated. Arithmetic averages allow us to generalize the humus content in soils. So, in the series of sod-podzolic soils – light gray forest-gray forest – dark gray forest-podzolic chernozems – leached chernozems-typical soils in a layer of 0-30 cm on average contains 2,20; 2,58; 3,76; 4,76; 6,8; 7,6; 7,2 % humus. The observed patterns of humus accumulation in soils are also preserved in the distribution of its reserves – 85; 97; 140; 162; 233; 257; 240 tons per he-1. It is proposed to characterize the general population along the boundaries of typical values that fit into the 50% confidence interval to assess the overall range of spatial variability of humus indicators. The upper limit of the typicity will correspond to the greatest accumulation of humus with a combination of local features of soil formation factors and can serve as a guide for predicting carbon sequestration in the soils of this region. Accordingly, the carbon-sequestering potential of sod-podzolic soil and typical chernozem is-20 tons per he-1, light gray forest soil-22 tons per he-1, gray forest soil and leached chernozem-27 tons per he-1, the highest values in dark gray forest soil are more than 30 tons per he-1
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Mamedzade, Vafa. "Microbiological Indicators of Meadow-Brown Soils of Natural Cenoses." Natural Systems and Resources, no. 3 (October 2021): 34–38. http://dx.doi.org/10.15688/nsr.jvolsu.2021.3.5.

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The article presents data on microbiological indicators of meadow-brown soils of semi-humid subtropics of the Lenkoran region. Meadow-brown soils are typical representatives of a number of hydromorphic soils of Azerbaijan. These soils are formed under sparse forests and shrub plantations with well-developed herbage. The soil-forming rocks are deluvial-proluvial deposits of clay composition. The influence of groundwater and surface runoff on soil formation is periodic. In the described soils, biological processes, including the activity of microorganisms, take place at moderate moisture level (10–25%) and temperature (18–23 °C). The paper presents a comparative analysis of the total number of microorganisms (in a layer of 0–50 cm) between typical meadow-brown, meadow-brown leached, meadow-gray-brown and gray-earth-meadow soils. We have shown changes in the total amount of microbiota for individual horizons of meadow-brown soils. Changes in the quantitative indicators of the microbiota of the studied soils also affect their overall biogenicity. A close relationship has been established between humus and the number of microorganisms. As the humus decreases in individual horizons, an adequate decrease in the number of microbiota is noted. If in 0–5 cm, 5–10 cm, 10–15 cm layers the amount of microbiota varied between 6,13–5,83–4,81 million per gram of soil, then in deeper layers of 15–20 cm, 20–25 cm, 30–40 cm, 35–50 cm, their number gradually decreases to 3,9–3,10–2,65–1,81–1,52 million per gram of soil.
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Kuziev, Jakhongir, Alisher Matyakubov, Shavkat Jumaev, and Sobirjon Nizamov. "Compatibility of ‘soil-variety-fertilizer’ to fertilizer norms and dynamics of food elements." E3S Web of Conferences 244 (2021): 02038. http://dx.doi.org/10.1051/e3sconf/202124402038.

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This article notes the geographical location and soil-climatic conditions of Kashkadarya province in Uzbekistan, as well as the mechanical composition, agrochemical properties and dynamics of nutrients in the soil of field experiments conducted in the conditions of typical irrigated gray soils in Shakhrisabz district. In total, 36% of the irrigated soils of the Kashkadarya basin are typical gray soils, and the genetic layers of the soils of the studied area are medium sandy, with large dust particles predominating in the mechanical fraction and create nutritional regimens. In the driving layers of the studied soils, humus 1.094%, total nitrogen 0.080%, total phosphorus 0.168%, total potassium 1.07%, mobile nitrogen, phosphorus and exchangeable potassium belong to low and moderately supplied groups. It is also possible to fully demonstrate the potential of cotton by creating a scientifically based nutrient environment for the promising variety “Porlok-4”.
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Bekhovykh, Yu V., and E. G. Sizov. "MORPHOLOGICAL STRUCTURE AND SOME AGROPHYSICAL PROPERTIES OF SANDY LOAM AND LOAMY GRAY FOREST SOILS OF THE BIE-CHUMYSH UPLAND UNDER THE BIRCH FOREST." Vestnik scientific and methodological council in environmental engineering and water management, no. 21 (2021): 46–50. http://dx.doi.org/10.26897/2618-8732-2021-21-46-50.

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The research goal was to study the morphological structure and some agrophysical properties of the gray forest soils of the Bie-Chumysh Upland under a birch forest. The study showed that under the birch forests, loamy and sandy loam soils were formed, belonging to the type of gray forest soils. All studied ag-rophysical characteristics are typical for this type of soil. The morphological structure also corresponds to the type of soil with clear signs of woody vegetation.
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Book chapters on the topic "Typical gray soils"

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Hale, Robert C., Meredith E. Seeley, Ashley E. King, and Lehuan H. Yu. "Analytical Chemistry of Plastic Debris: Sampling, Methods, and Instrumentation." In Microplastic in the Environment: Pattern and Process. Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-78627-4_2.

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AbstractApproaches for the collection and analysis of plastic debris in environmental matrices are rapidly evolving. Such plastics span a continuum of sizes, encompassing large (macro-), medium (micro-, typically defined as particles between 1 μm and 5 mm), and smaller (nano-) plastics. All are of environmental relevance. Particle sizes are dynamic. Large plastics may fragment over time, while smaller particles may agglomerate in the field. The diverse morphologies (fragment, fiber, sphere) and chemical compositions of microplastics further complicate their characterization. Fibers are of growing interest and present particular analytical challenges due to their narrow profiles. Compositional classes of emerging concern include tire wear, paint chips, semisynthetics (e.g., rayon), and bioplastics. Plastics commonly contain chemical additives and fillers, which may alter their toxicological potency, behavior (e.g., buoyancy), or detector response (e.g., yield fluorescence) during analysis. Field sampling methods often focus on &gt;20 μm and even &gt;300 μm sized particles and will thus not capture smaller microplastics (which may be most abundant and bioavailable). Analysis of a limited subgroup (selected polymer types, particle sizes, or shapes) of microplastics, while often operationally necessary, can result in an underestimation of actual sample content. These shortcomings complicate calls for toxicological studies of microplastics to be based on “environmentally relevant concentrations.” Sample matrices of interest include water (including wastewater, ice, snow), sediment (soil, dust, wastewater sludge), air, and biota. Properties of the environment, and of the particles themselves, may concentrate plastic debris in select zones (e.g., gyres, shorelines, polar ice, wastewater sludge). Sampling designs should consider such patchy distributions. Episodic releases due to weather and anthropogenic discharges should also be considered. While water grab samples and sieving are commonplace, novel techniques for microplastic isolation, such as continuous flow centrifugation, show promise. The abundance of nonplastic particulates (e.g., clay, detritus, biological material) in samples interferes with microplastic detection and characterization. Their removal is typically accomplished using a combination of gravity separation and oxidative digestion (including strong bases, peroxide, enzymes); unfortunately, aggressive treatments may damage more labile plastics. Microscope-based infrared or Raman detection is often applied to provide polymer chemistry and morphological data for individual microplastic particles. However, the sheer number of particles in many samples presents logistical hurdles. In response, instruments have been developed that employ detector arrays and rapid scanning lasers. The addition of dyes to stain particulates may facilitate spectroscopic detection of some polymer types. Most researchers provide microplastic data in the form of the abundances of polymer types within particle size, polymer, and morphology classes. Polymer mass data in samples remain rare but are essential to elucidating fate. Rather than characterizing individual particles in samples, solvent extraction (following initial sample prep, such as sediment size class sorting), combined with techniques such as thermoanalysis (e.g., pyrolysis), has been used to generate microplastic mass data. However, this may obviate the acquisition of individual particle morphology and compositional information. Alternatively, some techniques (e.g., electron and atomic force microscopy and matrix-assisted laser desorption mass spectrometry) are adept at providing highly detailed data on the size, morphology, composition, and surface chemistry of select particles. Ultimately, the analyst must select the approach best suited for their study goals. Robust quality control elements are also critical to evaluate the accuracy and precision of the sampling and analysis techniques. Further, improved efforts are required to assess and control possible sample contamination due to the ubiquitous distribution of microplastics, especially in indoor environments where samples are processed.
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Partoev, Kurbonali, Safarmadi Mirzoali, and Navruz Saidaliev. "Improving the Use of Land Resources in Tajikistan by Optimizing the Choice of Crops." In Ecological Aspects of Soil and Land Preservation. IGI Global, 2024. http://dx.doi.org/10.4018/979-8-3693-3374-7.ch004.

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Tajikistan's position in the desert zone, arid climate and mountainous terrain determined the characteristics of its soil cover. The soils mainly belong to the following types: light gray soils, typical gray soils, and mountain carbonate soils. In the Republic of Tajikistan, the total land fund or total land area is 14255.4 thousand hectares, of which 3746.0 thousand hectares are farmland. Over the past 30 years, the state of land resources in the Republic of Tajikistan has deteriorated. The share of irrigated land in relation to the area of ​​agricultural land/arable land decreased from 14.8% to 14.4%; area of ​​arable land per capita – from 0.16 to 0.12 ha/person. The share of agricultural land in relation to the total territory decreased by 1%. At the same time, there are natural limitations on the area of ​​land resources of 3746.0 thousand hectares of farmland. This actualizes the need for their effective and rational use. 90% of the area of ​​rain-fed arable land shows signs of degradation, of which 40% are highly degraded. Additionally, intensive agricultural activities on mountain slopes inevitably lead to soil erosion. They are eroded, which, as the gorges grow, leads to a reduction in the area of ​​arable soil. Slopes up to 250 m high are widely cultivated without anti-corrosion measures.
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Khan, Bushra Nisar. "Impact of Biochar on Soil Organisms." In Biochar - Solid Carbon for Sustainable Agriculture. BENTHAM SCIENCE PUBLISHERS, 2024. http://dx.doi.org/10.2174/9789815238068124010006.

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Soil organisms are very important to improve soil fertility and maintain a natural balance between soil nutrient cycles, enzyme activities and biological transformation of complex substances. Typically, one gram of soil contains more than 90 million bacteria, which helps plants in nutrient uptake by converting them into forms that are available to the plants. People tend to think negatively of microbes because they are unaware of how important they are, even though they frequently behave as disease-causing agents. Similarly, the role of soil macroorganisms in improving soil structure and nutrient movement is equally significant. The use of biochar as an exuberant carrier of soil organisms in the soil ecosystem has been widely studied. Therefore, in this chapter, we will emphasis the types and functions of macro and microorganisms in the soil, the impact of biochar on soil organisms, nutrient cycling and enzyme activities.
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Robinson, Mark. "The Geomorphology and Topography of the Area of the Porta Stabia Excavations." In The Porta Stabia Neighborhood at Pompeii Volume I. Oxford University PressOxford, 2023. http://dx.doi.org/10.1093/oso/9780192866943.003.0007.

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Abstract The topography of the Porta Stabia area is defined by geomorphology of the lava plateau of Pompeii, shaped by later volcanic events as well as by the natural north–south valley of the via Stabiana. The bedrock and paleosols in this area of the plateau had been heavily quarried and terraced in the course of later building activities, but typically were shallowest on the northeastern side of the site and deepest to the southwest. Sealing the lava bedrock was a level of yellow sandy silt resulting from the Mercato eruption of Vesuvius (7,000–6,700 bce). Above, a brown sandy silt attested to weathering and biogenic soil formation processes of this material. The project did not uncover any evidence of the Ante-Plinian gray ash that covers this soil elsewhere in Pompeii. There was no evidence for human presence in the area prior to the sixth-century bce foundation of the city, likely due to the presence of swampy marshland immediately south of the later Porta Stabia.
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Hay, Roderick J. "Nocardiosis." In Oxford Textbook of Medicine, edited by Christopher P. Conlon. Oxford University Press, 2020. http://dx.doi.org/10.1093/med/9780198746690.003.0135.

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Nocardia species—Nocardia asteroides, N. brasiliensis, and N. otidiscaviarum—are Gram-positive, filamentous, partially acid-fast bacteria. They are occasionally detectable in environmental sources such as soil, but they rarely cause infections in humans, although they can give rise to a variety of different diseases. In healthy individuals, most commonly in the tropics, they can present with cutaneous abscesses or subcutaneous infections (actinomycetoma) in which the organisms are present as clusters of filaments or grains. In immunocompromised patients they cause a disseminated or localized deep infection, with particular sites affected being the lungs or brain. Diagnosis of Nocardia infection depends on culture, although histopathology is very useful in Nocardia actinomycetomasiii. Antibiotic treatment is typically with a sulphonamide (often as co-trimoxazole for lung infections), but combinations of drugs are usually given because the responsiveness of Nocardia species is very variable.
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Conference papers on the topic "Typical gray soils"

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Zamanzadeh, Mehrooz, Edward Larkin, Peyman Taheri, et al. "Water Main Breaks - High Time to Learn from Mistakes and Avoid Further Breaks." In CORROSION 2021. AMPP, 2021. https://doi.org/10.5006/c2021-16837.

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Abstract Water main failures are very expensive for municipalities because they typically result in expenses associated with repair costs, flood damage, and loss of revenue to affected businesses. Water main failures also interrupt the operation of vital services, such as medical care and fire-fighting operations. Currently, millions of dollars are spent annually by the water utility industry and by municipalities on the repair of failed components of the water distribution infrastructure, such as components that are made from gray cast iron or "gray iron” pipe and ductile cast iron or "ductile iron” pipe. The rate of municipal water main failures is expected to increase as the existing cast iron infrastructure continues to age. The cost of repairing damages caused by broken water mains (and subsequent flooding damage) may become an important item in many municipal budgets. It is important to develop a corrosion program to prevent catastrophic failures of water mains. This paper presents a plan consisting of several phases including preassessment, indirect assessment, direct assessment, and integrity assessment of failed water mains. We will elaborate on the failure mechanisms, failure analysis protocols, and corrosion mitigation strategies for water mains that experience breaks. Water main breaks are mainly due to corrosive soil, pipe material, galvanic action, stray current corrosion, or microbiological induced corrosion (MIC). This paper provides an overview of corrosion issues commonly experienced by water main pipes, presents specific case histories involving graphitic corrosion, galvanic corrosion, stray current corrosion, and MIC. In this paper, we will introduce a graphitization sensor for condition assessment of water mains. This sensor can identify the location and extent of graphitization on water main.
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Onorato, George. "DFI Technical Committee Project on the Effect of Overburden Stresses (During Curing) on the Mechanical Properties of Soil-Cement Mixed Materials." In Deep Foundations Institute 49th Annual Conference. Deep Foundations Institute, 2024. https://doi.org/10.37308/dfi49.2024610109.

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Deep soil mixing (DSM) has become a widely used ground improvement technique globally, producing soil-cementitious materials for various complex civil and environmental applications. In the field, the soil-cement materials form under confining stress conditions, which are often overlooked, as most wet grab specimens are cured and tested under ambient atmospheric conditions. This oversight has led to an underestimation of the engineering and mechanical properties of the soil-cement mixed material. With support from the DFI Technical Committee Project Fund, the authors initiated a multi-phased comprehensive research study in collaboration with industry experts to gain a fundamental understanding of these effects. This study investigates the curing conditions to which in-situ materials are exposed and how these conditions influence the strength of deep mixed materials. The findings reveal that the curing conditions for in-situ materials, including applied stresses and temperatures, significantly differ from those under which typical quality control specimens are cured. Neglecting these conditions can lead to a substantial underestimation of in-situ material strength. The data compiled for this study encompass strength and temperature data obtained from specially designed laboratory bench tests, field-conducted modified oedometer tests, in-situ instrumentation tests within deep mixed columns, and a review of independent coring data from deep mixed projects across North America. Analysis of these collective studies reveals a correlation between curing stress and unconfined compressive strength (UCS). The rate of strength gains follows a linear pattern and is influenced by the soil type being treated. Fine-grain soils, in particular, exhibit a higher rate of strength gain when subjected to in-situ curing stress (with depth) compared to granular soils. The paper delves into fundamental processes such as drainage, consolidation, and interparticle behaviors of deep mixed materials from their fresh state until the treated column has cured. It also presents empirical and analytical methods to correct in-situ strength measurements to account for the effects of curing stresses.
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