Academic literature on the topic 'Loess-like'

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Journal articles on the topic "Loess-like"

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Zhang, Ming, Bao Ming Wang, and Song Jiang Wang. "Correlation Analysis of CPT Parameters and the Physico-Mechanical Parameters of the Loess-Like Silty Clay Soil." Applied Mechanics and Materials 482 (December 2013): 26–29. http://dx.doi.org/10.4028/www.scientific.net/amm.482.26.

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The cone penetration test (CPT) for loess-like silty clay soil in western Henan province was done to obtain the tip resistance and sleeve friction. Then, the relationship of CPT and physico-mechanical parameters of loess-like silty clay soil was analysis. At last, the empirical model for physico-mechanical parameters of loess-like silty clay soil in western Henan province was established. The physico-mechanical parameters of loess-like silty clay in western Henan province could be calculated by sing the empirical model from CPT, including water content, void ratio, plasticity index and compres
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GARCÍA, R., M. D. PETIT-DOMÍNGUEZ, M. I. RUCANDIO, and J. A. GONZÁLEZ. "Provenance of loess from the Spanish central region: chemometric interpretation." Geological Magazine 148, no. 3 (2010): 481–91. http://dx.doi.org/10.1017/s0016756810000889.

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AbstractIn this work our purposes are (1) geochemical characterization of loess (‘primary loess’ or ‘true loess’ and ‘secondary loess’ or ‘loess-like deposits’) located in the centre of the Iberian Peninsula, (2) systematic study of element behaviour during pedogenesis and (3) evaluation of the suitability of using the geochemistry of loess to establish the average composition of these discontinuous aeolian sedimentary covers in central Spain. Several analyses were carried out on the bulk sample and on the sandy and clay fractions (mineralogical composition by X-ray diffraction, mineralogical
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Korobova, Olga, and Ljubov Maksimenko. "Study loess and loess-like rocks primer of the Western Siberia." E3S Web of Conferences 431 (2023): 09006. http://dx.doi.org/10.1051/e3sconf/202343109006.

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Recently, the development problems of the loess subsidence soils as foundations of buildings and structures arise due to climate change on the planet in the consequence to the expansion of human economic activity and other unfavorable factors. For foundations composed of loess subsidence soils, the properties’ prediction is of great importance, taking into account the risks of flooding of territories, modern technologies for setting up foundations in already built-up and newly developed territories. Errors in design can contribute to a significant decrease in the values of strength and deforma
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Paktovsky, Y. G. "Loess doll from Pleistocene loess-like sediments in the Vishera diamond-bearing area (Perm region)." Vestnik of North-Eastern Federal University Series "Earth Sciences", no. 1 (March 25, 2024): 31–38. http://dx.doi.org/10.25587/2587-8751-2024-1-31-38.

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The purpose of the study is to investigate the cranes from loess-like deposits as indicator formations for the glacial epochs of the late Pleistocene – Holocene using current lithology methods. The motivating reason for the study was that loess-like deposits directly “seal” the industrial placer of the Silurian diamond-bearing reservoir in the Vishera diamondiferous region.Loess doll (loess pupae, dutiki) are concretions weakly cemented by iron hydroxides, consisting of quartz grains with an admixture of fine-silty feldspars. In terms of granulometry and mineral composition, the cranes corresp
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Vasiliev Oleg Alexandrovich, Semenov Vladimir Grigoryevich, Tuleubayev Zhaxybay, et al. "LOESS LIKE LOAMS AS A SOIL FORMATION FACTOR FOR LIGHT-GRAY FOREST SOILS IN THE CHEBOKSARY REGION OF THE CHUVASH REPUBLIC." BULLETIN 6, no. 388 (2020): 38–45. http://dx.doi.org/10.32014/2020.2518-1467.180.

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Covering loess-like loams are widespread in the Chuvash Republic and serve as parent rocks. They are heterogeneous both in the course and in the depth of occurrence. A distinctive feature of loess like loams from other overlying quaternary deposits is a sharp predominance in the granulometric composition of coarse dust fractions ranging in size from 0.05 to 0.01 mm, the content of which is 40% or more. Their granulometric composition varies from light loamy to clayey. Loess like loams, due to the peculiarities of their granulometric composition, have relatively good water permeability and mois
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Smalley, Ian, John Marshall, Kathryn Fitzsimmons, W. Brian Whalley, and Samson Ngambi. "Desert loess: a selection of relevant topics." Geologos 25, no. 1 (2019): 91–102. http://dx.doi.org/10.2478/logos-2019-0007.

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Abstract In discussions on loess, two types are often demarcated: glacial loess and desert loess. The origin of the idea of desert loess appears to lie with V.A. Obruchev who observed wind-carried silt on the Potanin expedition to Central Asia in 1895. It might be considered that desert loess would be defined as loess associated with deserts but it came to be thought of as loess produced in deserts. This led to some controversy as no mechanism for producing silt particles in deserts was readily available. Bruce Butler in Australia in particular cast doubt on the existence of desert-made loess.
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Romanescu, Gheorghe, Denes Lóczy, József Dezső, and Donatella Carboni. "Loess-Scape in the Dobrudja Plateau (Romania). Landforms and Updated Typology." Present Environment and Sustainable Development 12, no. 1 (2018): 95–114. http://dx.doi.org/10.2478/pesd-2018-0008.

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Abstract The study of loess and loess-like deposits in Romania has developed considerably, over the years. C14 dating determined that the last three glaciations (Mindel, Riss, Würm) and, at least, two interglacial periods were recorded in the Dobrudja Plateau. Five other paleosol layers indicate the succession of the Quaternary interglacial stations. The loess of Dobrudja, is about 50 m in thickness. The term loess-scape is comprised of all the processes and forms specific to these deposits, which create a unique landscape, with local peculiarities. Natural and anthropic conditions created loe
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Thamó-Bozsó, Edit. "Heavy mineral composition of some loess and loess-like sediments in Hungary." Quaternary International 279-280 (November 2012): 489. http://dx.doi.org/10.1016/j.quaint.2012.08.1661.

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Popov, S. S., G. N. Shilova, and A. O. Khotylev. "Area of distribution and conditions of loess forming in the South Urals." Moscow University Bulletin. Series 4. Geology, no. 6 (December 28, 2020): 16–30. http://dx.doi.org/10.33623/0579-9406-2020-6-16-30.

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The report presents the results of comprehensive studies of loess-like formations that are common within drainage basins of Ay and Yuruzan rivers (South Urals). Loess complexes associated with the third fluvial terrace. The lithological composition, structural and textural features indicate that the loess were formed like the part of alluvial fans, planned under the third fluvial terrace. The obtained palynological data indicate the formation of deposits in the Middle Pleistocene during the Odintsovo interglacial and Moscow glaciation.
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Goryukhin, M. V. "NON-TRADITIONAL NATURAL RAW MATERIALS FOR THE MANUFACTURE OF PORCELAIN." Regional problems 26, no. 3 (2023): 66–71. http://dx.doi.org/10.31433/2618-9593-2023-26-3-66-71.

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The accumulated knowledge about the structure of a substance makes it possible to control its properties, including the purposeful selection of raw materials and materials for its creation, and vice versa, based on the natural or artificial material composition, predict its physical and chemical properties. This approach allows choosing a replacement for rare or even scarce types of mineral raw materials to produce a particular product. The analysis of literature data and sources, a comparative analysis of the Middle Amur Lowland loess-like rocks chemical composition, and one of the white porc
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Dissertations / Theses on the topic "Loess-like"

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Parks, D. A. "TL dating and geochemistry of brickearths in S.E. England." Thesis, University of Sussex, 1989. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.282705.

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Damane, Monica. "An investigation into the volume change characteristics of loess like soil in Mount Moorosi Village in Lesotho." Master's thesis, Faculty of Engineering and the Built Environment, 2019. http://hdl.handle.net/11427/31497.

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The Mount Moorosi village is situated in the Senqu River Valley of southern Lesotho, within the Stormberg landform. The integrity and aesthetic appearance of nearly all the structures in this area are undermined by recurrent cracks. At present, no apparent institutionalised effort had been conducted to investigate the source of this problem. The crack patterns were associated with the possible volume change of the underlaying loess like soil. This soil has caused a disastrous failure to brittle civil engineering structures in various parts of the world. Its behaviour is attributed to sand and
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Books on the topic "Loess-like"

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Różycki, Stefan Zbigniew. Loess and loess-like deposits: Evolution of views on the genesis of loess, classical loess provinces, loess of the warm zone. Ossolineum, 1991.

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Różycki, Stefan Zbigniew. Loess and loess-like deposits: Evolution of views on the genesis of loess, classical loess provinces, loess of the warm zone. Ossolineum, The Publishing House of the Polish Academy of Sciences, 1991.

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Engineering geological research of loess and loess-like sediments in the USSR: Review and bibliography. Geographical Research Institute Hungarian Academy of Sciences, 1987.

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Quaternary loesses, loess-like sediments, soils and climate change in Iran. Gebrüder Borntraeger, 2010.

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Book chapters on the topic "Loess-like"

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"Dish-Like Depression Landscape On Loess." In Dictionary of Geotourism. Springer Singapore, 2019. http://dx.doi.org/10.1007/978-981-13-2538-0_520.

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Bjornstad, Bruce N., Eugene P. Kiver, and Chad J. Pritchard. "Ice Age megafloods through the Cheney-Palouse Scabland Tract, eastern Washington, USA." In Proterozoic Nuna to Pleistocene Megafloods: Sharing Geology of the Inland Northwest. Geological Society of America, 2024. http://dx.doi.org/10.1130/2024.0069(08).

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ABSTRACT A two-day, ~300-mile field trip follows the path of ancient Ice Age megafloods through the eastern Channeled Scabland plexus and explores abundant evidence for the last outburst floods from the late Pleistocene within the Cheney-Palouse Scabland Tract, Washington, USA. Features unique to the scablands include spectacular, headward-retreating cataract canyons; giant ripples, bars, and scour holes along with dry waterfalls; battleship-sized, streamlined loess islands; and anastomosing channel networks. Some noteworthy flood features within the Cheney-Palouse tract include a massive 530-
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Das, Pankaj, and Samir Barman. "Perspective Chapter: An Overview of Time Series Decomposition and Its Applications." In Applied and Theoretical Econometrics and Financial Crises [Working Title]. IntechOpen, 2025. https://doi.org/10.5772/intechopen.1009268.

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Time series (TS) data is ubiquitous in various fields such as finance, economics, meteorology, and engineering. The analysis of TS data aims to understand the underlying patterns, make predictions, and inform decision-making. One of the fundamental techniques in TS analysis is decomposition, which breaks down a TS into its constituent components: trend, seasonality, and residuals. This chapter provides a comprehensive overview of TS decomposition, breaking down data into trend, seasonality, and residuals. It covers classical methods, such as additive and multiplicative models, advanced techniq
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Vicente, E., A. Krumb, and F. Ulbricht. "Difficult behavior of young continental “loess – like” clayey soil deposits of mud-volcanogenetic heritage in Azerbaijan." In Energy Geotechnics. CRC Press, 2016. http://dx.doi.org/10.1201/b21938-21.

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Rögner, KonraD, and WerneR Smykatz-Kloss. "The fine-grained, loess-like sediments of the Wadi Firan, Sinai, Egypt: Possibilities of palaeoclimatic interpretations?" In Quaternary Deserts and Climatic Change. CRC Press, 2020. http://dx.doi.org/10.1201/9781003077862-22.

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Conference papers on the topic "Loess-like"

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Paktovsky, Yu G. "Loess-like deposits of the diamond-bearing placer Yuzhnaya Rassolnaya (Perm region)." In Problems of mineralogy, petrography and metallogeny. Scientific readings in memory of P.N. Chirvinsky. Perm State University, 2024. http://dx.doi.org/10.17072/chirvinsky.2024.107.

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The article describes the loess-like deposits of the northwestern blocks of the South Rassolnaya deposit, where the industrial diamond content of the Silurian intermediate reservoir was previously established. In these proposals of field geologists, «cranes» (loess pupae, loess nodules, dutiki) are noted. The article studied: 1) the granulometric composition of loess-like deposits using two methods: sieve analysis and laser diffraction analyzer Analysette 22 MicroTec plus; 2) the mineral composition of the heavy fraction of loess-like and underlying sediments - using quantitative mineralogical
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Nurgalieva, Kamilya, Assyl Bissengaliyeva, Akmaral Kassymova, Aibek Kuldybayev, and Aina Taskairova. "Effect of microwave fields on loess-like loams." In Third International Scientific and Practical Symposium on Materials Science and Technology (MST-III 2023), edited by Ramazon Abdullozoda and Shahriyor Sadullozoda. SPIE, 2024. http://dx.doi.org/10.1117/12.3017738.

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Gaudenyi, Tivadar. "LOESS OF SERBIA—FROM PALEOCLIMATE TO WINEYARDS." In Book of Abstracts and Contributed Papers. Geographical Institute "Jovan Cvijić" SASA, 2024. http://dx.doi.org/10.46793/csge5.05tg.

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Loess is a buff colored, clastic sedimentary rocky of eolian origin without stratification and laminations where the silt particles predominates (beside clay and sand). Gentle lithification with carbonate bonds makes them highly sensitive to water impacts which dissolute this rock. Its vertical breaking made steep slopes. Loess in the sedimentary record deposits are not homogenous sediments, but most contain paleosols or sand horizons which we denominated loess series or loess-paleosol sequences. In Serbia loess series are the most widespread eolian sediments on which the high quality chernoze
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Mouraviev, Fedor, Tatyana Kropotova, Bulat Gareev, Georgi Batalin Alexander, and A. Gordeev. "LOESS-LIKE SILTSTONES FROM THE URZHUMIAN (MIDDLE PERMIAN) RED BEDS OF KAZAN VOLGA REGION, RUSSIA." In 20th SGEM International Multidisciplinary Scientific GeoConference Proceedings 2020. STEF92 Technology, 2020. http://dx.doi.org/10.5593/sgem2020/1.1/s01.020.

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