Academic literature on the topic 'Differential weathering'

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Journal articles on the topic "Differential weathering"

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White, Art F., Thomas D. Bullen, Marjorie S. Schulz, Alex E. Blum, Thomas G. Huntington, and Norman E. Peters. "Differential rates of feldspar weathering in granitic regoliths." Geochimica et Cosmochimica Acta 65, no. 6 (March 2001): 847–69. http://dx.doi.org/10.1016/s0016-7037(00)00577-9.

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Deng, Zhiyong, Fengchong Lan, and Jiqing Chen. "Differential Distribution Analysis and Region and Grade Regulation on Auto-Parts Weathering External Factors with Non-Uniform Thermal Environment." Applied Sciences 10, no. 15 (July 25, 2020): 5116. http://dx.doi.org/10.3390/app10155116.

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It is difficult to comprehensively master and precisely regulate the external factors distribution of automobile weathering in non-uniform thermal environment as well as the consequent disequilibrium weathering problem, while exploring weather-resistant materials in uniform thermal environment. Thus, a numerical calculation method for the weathering external factors is proposed, on the basis of annual experimental study on the outdoor weathering inconsistencies of auto-parts. The time–space distribution characteristics and day–night variation rules of the external factors are studied, and the disequilibrium weathering mechanism among parts is revealed from the perspective of non-uniform distribution of external factors. The laws of automotive physical parameters, orientations and locations, as well as their influences on external factors distribution are analyzed in detail, and hereby the targeted schemes to effectively reduce the local external factor intensity and the thermal gradient between parts are investigated. The method can be used to rapidly predict weathering external factors distribution of vehicle exposed to outdoor in any direction during day and night, so as to provide auto-parts with differentiated test schemes in accelerated tests and IP/DP box tests, and it also contributes to present some pertinence guidance for the accurate regulation of automobile disequilibrium weathering on regions at different levels.
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Guo, Yan Fen, You Ji Tao, Gan Xin Jie, Jun Wang, Xiao Dong Zhang, Li Fen Hu, and Xin Liu. "Degradation Behavior of Pure Polystyrene Subjected to Two Natural Climate Types and the Simulated Effect of Artificial Accelerated Weathering." Applied Mechanics and Materials 713-715 (January 2015): 2632–39. http://dx.doi.org/10.4028/www.scientific.net/amm.713-715.2632.

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Pure polystyrene (PS) was subjected to natural weathering in Qionghai (QH) and Ruoqiang (RQ) of China, representing hot and humid climate and xerothermic climate respectively. The degradation profile of pure PS was studied by Fourier Transform Infrared (FTIR) Spectroscopy, Differential Scanning Calorimetry (DSC), Scanning Electron Microscope (SEM), X-ray Photoelectron Spectroscopy (XPS) and Spectrophotometer. Artificial accelerated weathering tests protocol A and B were carried out to simulate hot and humid climate and xerothermic climate respectively. Results show that pure PS degrade slowly at the initial stage and then become faster. Color shift could be an appropriate indicator for evaluating simulated effect of artificial accelerated weathering and protocol A simulate hot and humid climate perfectly while protocol B turns out weak for xerothermic climate.
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McCarroll, Danny. "Differential weathering of feldspar and pyroxene in an arctic-alpine environment." Earth Surface Processes and Landforms 15, no. 7 (November 1990): 641–51. http://dx.doi.org/10.1002/esp.3290150706.

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Ibarra, Daniel E., Jeremy K. Caves, Seulgi Moon, Dana L. Thomas, Jens Hartmann, C. Page Chamberlain, and Kate Maher. "Differential weathering of basaltic and granitic catchments from concentration–discharge relationships." Geochimica et Cosmochimica Acta 190 (October 2016): 265–93. http://dx.doi.org/10.1016/j.gca.2016.07.006.

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Andersson, P. O. D., and R. H. Worden. "Stratigraphic variations in mudstone mineral assemblages from a submarine fan-complex: Karoo Basin, South Africa." Clay Minerals 41, no. 4 (December 2006): 839–52. http://dx.doi.org/10.1180/0009855064140223.

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AbstractDespite the high-grade diagenesis experienced by the Skoorsteenberg Formation mudstones, Tanqua Karoo basin, South Africa, geochemical data have been interpreted to reveal primary mineralogy and so help understand provenance evolution. The geochemical signatures show systematic variations related to stratigraphy. The main changes in mudstones from the lower to the upper part of the section include: (1) an increase in the feldspar content of the primary sediment and a decrease in the content of Al-rich clay (probably dioctahedral smectite); (2) a decrease in the degree of chemical weathering of the sediment, representing a change to a dryer and/or cooler climate; (3) an increase in TiO2/Al2O3 representing increasing mafic sources; (4) an increase in CaO/(K2O+CaO) also possibly representing increasing mafic sources. Mass flux and differential diagenesis are unlikely to be responsible for the depth-related changes since the rocks have undergone the same degree of high-grade diagenesis and the mudstones are interrupted by other lithologies, so disturbing any sort of diffusion gradient. These variations could plausibly be the result of one or more of differential weathering, evolving provenance characteristics or variable hydrodynamic fractionation of the sediment. The ratio of Zr/Y, a possible indicator of hydrodynamic fractionation, increases only slightly and irregularly up-section. There is no relationship between the silica content, representative of the quartz-silt content of the sediment, and TiO2/Al2O3 showing that the amount of quartz, and so the degree of hydrodynamic fractionation, has not controlled mudstone geochemistry. The stratigraphic increase in feldspar content, the decrease in Al-rich clay content and increase of both TiO2/Al2O3 and CaO/(K2O+CaO) must be due to a combination of marginally evolving provenance characteristics (more mafic and felsic rocks exposed to weathering with time) and changes in the degree of rock weathering (less chemical weathering with time).
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Zhu, Tengwei, Feng Huang, Jing Liu, Qian Hu, and Wei Li. "Effects of inclusion on corrosion resistance of weathering steel in simulated industrial atmosphere." Anti-Corrosion Methods and Materials 63, no. 6 (November 7, 2016): 490–98. http://dx.doi.org/10.1108/acmm-05-2015-1538.

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Purpose This paper aims to investigate the atmospheric corrosion mechanism of structural materials to develop more advanced corrosion-control technologies and cost-reduction strategies. As a second phase in steels, the non-metallic oxide inclusions are considered to not only affect the mechanical properties of steel but also the corrosion resistance of steel. So, an important research goal in this paper is to investigate the indoor accelerated corrosion kinetics of Q450NQR1 weathering steel, analyzing the galvanic polarity of different inclusions in electrochemical corrosion microcell between the inclusion and steel matrix and then elucidating the influence mechanism of inclusions on corrosion resistance of weathering steel. Design/methodology/approach Two methods of inclusion modification are usually used to improve the properties of weathering steel: one is calcium treatment on aluminum killed steel and the other one is rare earth (RE) modification. Wet/dry cyclic immersion corrosion test field emission scanning electron microscopy (FE-SEM) metallographic optical microscope. Findings The indoor accelerated corrosion kinetics of Q450NQR1 weathering steel could be divided into two stages with different log (thickness loss, D)-log (time, t) fitting functions, and the effect of inclusions on the corrosion resistance of Q450NQR1 weathering steel was only reflected in the initial stages of corrosion. The inclusions of CaS in Ca-modified test steel and RE oxides and sulfides in RE-modified test steel were preferentially dissolved in acid media, slowing down the corrosion rate of steel matrix, but the non-metallic inclusion Al2O3 may accelerate the corrosion rate of the steel matrix as a form of differential aeration corrosion. Originality/value The effects of inclusions on corrosion resistance of Q450NQR1 weathering steel was investigated by dry–wet cycle immersion test and FE-SEM. The effect of inclusions on the corrosion resistance of Q450NQR1weathering steel was only reflected in the initial stages of corrosion. The inclusions of CaS in Ca-modified test steel and rare earth (RE) oxides and sulfides in RE-modified test steel were preferentially dissolved in acid media, slowing down the corrosion rate of steel matrix, but the non-metallic inclusion Al2O3 may accelerate corrosion rate of the steel matrix as a form of differential aeration corrosion.
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Darmody, Robert G., Colin E. Thorn, and John C. Dixon. "Differential rock weathering in the ‘valley of the boulders', kärkevagge, swedish lapland." Geografiska Annaler: Series A, Physical Geography 90, no. 3 (September 2008): 201–9. http://dx.doi.org/10.1111/j.1468-0459.2008.339.x.

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Todisco, Dominique, and Hervé Monchot. "Bone Weathering in a Periglacial Environment: The Tayara Site (KbFk-7), Qikirtaq Island, Nunavik (Canada)." ARCTIC 61, no. 1 (March 1, 2009): 87. http://dx.doi.org/10.14430/arctic9.

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Bone weathering analysis of the Palaeoeskimo Tayara site (Qikirtaq Island, Nunavik, Canada) documents site taphonomy in the Arctic periglacial environment. Like a majority of sites in the eastern Canadian Arctic, Tayara has a faunal assemblage dominated by marine mammals (seal, walrus, and beluga whale) and some terrestrial mammals (caribou, fox, and bear). Statistical and spatial analyses of five weathering stages reveal that large mammal bone preservation is generally good and does not seem to be influenced by taxonomic and skeletal differences. The good preservation of the faunal assemblage seems to have been favored by the burial of bones and their incorporation into the active layer, which suggests only limited mechanical deterioration (i.e., freeze-thaw or wet-dry cycles, or both) before or at the time of burial. Burial depth partly explains the degree of bone weathering. Indeed, the well-preserved bones are found mainly where burial is associated with thicker overlying sediments. This implies rapid bone burial with a low degree of exposure to temperature changes and atmospheric processes. However, analysis also shows the presence of highly weathered bones where burial is associated with thicker overlying sediments. Consequently, differential bone depth probably does not explain all bone-weathering variability within the site. These results show the importance of examining bone weathering before any archaeozoological and paleoethnographic interpretations.
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Butylina, Svetlana, Marko Hyvärinen, and Timo Kärki. "Weathering of wood-polypropylene and wood-wollastonite-polypropylene composites containing pigments in Finnish climatic conditions." Pigment & Resin Technology 44, no. 5 (September 7, 2015): 313–21. http://dx.doi.org/10.1108/prt-08-2014-0066.

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Purpose – The purpose of this paper is to study the resistance of wood-polypropylene and wood-wollastonite-polypropylene composites containing pigments to natural weathering. Design/methodology/approach – Natural weathering of composites was conducted in Finnish climatic conditions for one year. The colour of the composites was determined with a spectrophotometer, the morphology of the composite surface was analysed by scanning electron microscopy (SEM), and the changes in the polymer structure in surface layer of the composites were analysed with differential scanning calorimetry (DSC). Charpy impact strength was determined with an impact tester. Findings – The pigments used in this study reduced the colour change of the composites exposed to outdoor weathering as compared with the un-coloured composite. The carbon black pigment was more effective than the iron oxide pigment. Moreover, only the carbon black pigment was found to reduce the degradation of the surface layer of the composites. The addition of the carbon black pigment had a positive effect on the dimensional stability of the composites in a water absorption test. Only the combination of the carbon black pigment and wollastonite resulted in a composite which was capable to retain its Charpy impact strength both after one year of outdoor weathering and cyclic treatment. Research limitations/implications – This study is a part of continuous research on the development of wood-polymer composites (WPUs) suitable for outdoor applications in Finnish climatic conditions. The first part of the study, which has been published earlier, showed the results of weathering of composites in accelerated tests in comparison with 1,000 hours outdoor exposure during summer time (June and July). Outdoor weathering limited to 1,000 hours cannot give an objective view on the weathering behaviour of composites in Finnish climatic conditions. The results of the current study were obtained from one-year outdoor exposure of composites. Originality/value – The wood-polypropylene composite made with the combination of the carbon black pigment and wollastonite can be recommended for outdoor applications. The study provides useful information on the resistance of wood-polypropylene composites to weathering in Finnish climatic conditions.
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Dissertations / Theses on the topic "Differential weathering"

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Ploger, Desiree. "Effects of ultraviolet (UV) radiation on thermal, chemical, and rheological properties of rubber-modified asphalt binders." Master's thesis, Alma Mater Studiorum - Università di Bologna, 2018.

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This research aims to investigate the thermal, chemical and rheological properties of UV-aged asphalt binders containing recycled tire rubber (RTR) powder. The UV Aging process changes the chemical composition and physical properties of asphalt and causes distress on pavement. It is known that the presence of crumb rubber (CR) reduces the susceptibility of asphalt to aging, but its mechanism is not fully understood. Moreover the rheological performance of a crumb rubber modified binder are still partially unknown. In this research, the effect of ultraviolet (UV) rays on samples of asphalt binder mixed with crumb rubber is studied. One neat binder and two sets of rubber-modified samples with 16.6 and 20 %wt. are prepared and then inserted inside a QUV Accelerated Weathering Tester for 100 hours. The samples are then collected and changes in their thermal conductivity, chemical indices and rheology are studied using Nanoflash, differential scanning calorimeter, FTIR, and dynamic shear rheometer (DSR), respectively. Results show that addition of rubber leads to a reduction of specific heat for the two rubberized binders. Specific heat capacities of the three UV aged samples are larger than those of their unaged counterparts, and the 16.6%-aged has the highest value. FTIR spectra of the three unaged samples are very similar, whereas distinct changes occur after UV aging. The normalized absorbance of peak associated with S=O group increases and the peak for the aliphatic group decreases after UV aging, showing some evidences of oxidation due to UV aging. Using crumb rubber in the binder decreases the thermal conductivity and 20% wt. sample is even less conductive compared to the 16.6%wt. At all temperatures above 25°C, aged samples have lower thermal conductivity than the unaged ones, except neat binder which was opposite. Rheological measurements show that complex modulus of the samples increases with addition of rubber particles and also aging.
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Bitom, Dieudonné. "Organisation et évolution d'une couverture ferralitique en zone tropicale humide (Cameroun) : génèse et transformation d'ensembles ferrugineux indurés profonds." Poitiers, 1988. http://www.theses.fr/1988POIT2327.

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On etudie la couverture ferralitique rouge de la zone forestiere du sud cameroun du point de vue petrographique, mineralogique, geochimique et cristallochimique. Son evolution correspond a deux mecanismes de pedogenese, l'une a l'amont a evolution verticale descendante, l'autre a l'aval a evolution verticale ascendante, cette derniere du niveau de la nappe phreatique
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Godon, Nicole. "Effet des materiaux d'environnement sur l'alteration du verre nucleaire r7t7 : influence des argiles." Orléans, 1988. http://www.theses.fr/1988ORLE2045.

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On a entrepris des essais comparatifs sur differents materiaux argileux et on a suivi la cinetique de l'interaction eau/verre/materiau pendant 1 an. La presence d'argile a ete correlee avec la vitesse de corrosion du verre nucleaire et on a recherche le meilleur materiau pour elaborer des barrieres ouvragees empechant cette alteration
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ATASSI, HANAE. "Evaluation de la resistance a la corrosion en solution aqueuse de quelques verres silicates." Université Louis Pasteur (Strasbourg) (1971-2008), 1989. http://www.theses.fr/1989STR13057.

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Des experiences ont ete realisees afin d'evaluer la resistance chimique de verres volcaniques et industriels, mis en contact avec de l'eau distillee et des solutions tampons a ph 6, 7, 8 et 9. On a etudie au microscope electronique les couches d'alteration en surface et les resultats ont ete compares a un modele cinetique de la dissolution du verre ainsi qu'a un modele thermodynamique (modele de paul)
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Conca, James Louis. "Differential Weathering Effects and Mechanisms." Thesis, 1985. https://thesis.library.caltech.edu/1284/1/Conca_jl_1985.pdf.

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The physical and chemical characteristics of the two differential weathering effects, case hardening and core softening, are examined to determine their formation mechanisms by investigating several field areas exhibiting differential weathering effects. The terms differential weathering effects, factors, mechanisms, processes, morphologies and their cause and effect relationships are defined in the context of the overall problem.

Because differential weathering effects are defined on the basis of spatial variations in relative and absolute hardness, a portable field instrument has been developed to measure rock hardness as manifested in the abrasion resistance of the material.

The design and operation of the instrument as well as results from standard materials are discussed in light of abrasive wear theory. The way in which the instrument removes material appears dominated by abrasive wear mechanisms. However, the concept of hardness implied by such mechanisms is profoundly different for rock than for homogeneous materials, and the effective hardness calculated for rock material using this instrument is more insensitive to mineralogy than expected, and is sensitive to the character of the intergranular bond.

At the first locality, Valley of Fire, Nevada, cavernous weathering of the Aztec Sandstone results from the differential weathering effect of case hardening. The case-hardened crust is an induration phenomenon consisting primarily of host rock, calcite cement, kaolinite and finegrained quartz. The calcite occurs in a wide range of concentrations (0.001 to 5.0 wt%). The hydrated calcium borate, colemanite, was also found as a non-cementing hardening agent on two outcrops and can be used as a tracer constituent. In all cases kaolinite and quartz were the major constituents of the indurating materials by weight and are necessary components of the crust. Eolian deposition and interaction with meteoric water were determined to be the primary differential weathering mechanism within the Valley of Fire.

At Catavina, Baja California, tonalite exhibiting cavernous weathering is found to be core-softened. Soft cores are more chemically weathered than the exterior rock as indicated by higher kaolinite contents. Hematite formed from the leaching of biotite occurs in coatings on rock surfaces, but the hardening effect of the coating is insignificant compared to the core-softening of the interior. The hardness, measured by the abrasion resistance hardness tester, is inversely correlated with kaolinite content in the tonalite. A one-dimensional water flow model was developed for core-softened, cavernously weathered boulders, and indicates that during infiltration and dessication the moisture flux through a boulder's surface is greatest at the interior cavern wall because of changes in the hydraulic conductivities induced by core softening.

The differential weathering effects developed in the Ferrar dolerite within the Labyrinth of the Dry Valleys, Antarctica are caused by two different mechanisms. The primary mechanism is precipitation of a brown, iron-stained silica coating in the exterior rock of outcrops and joint blocks. This is also true for the case-hardened Beacon Sandstone. Precipitation can occur in the rock's outer few millimeters to centimeters, thereby decreasing the exterior rock's permeability, and consequently its susceptibility to chemical weathering. The coating's effect on a dolerite block's internal moisture regime is modeled for the case of saturated flow, and shows that the contours of the pore water flow mimic subsequent morphology. Weathering of material underlying the coating results in core softening of the dolerite. In dolerite blocks of intermediate size, expansion of the interior owing to weathering can cause the less weathered outer zone to separate into an array of polyhedral cracks. Further weathering and removal of the underlying rock by the combined action of hydration, salt weathering and eolian processes leads to the development of cavernous weathering.

A less common differential mechanism occurs in the bottom of the Antarctic Labyrinth troughs in which an eolian polish develops on rock surfaces exposed to the austral winter winds. Development of the polish protects the underlying material with similar, but less dramatic effects, than accompanies the presence of the silica coating.

Exposures of the Bishop Tuff in the Mono Basin exhibit the differential weathering effect of case hardening. Early devitrification along joint planes to an average depth of 1 cm greatly increased the resistance of the joint faces to weathering over that of the joint block interiors. The absolute and relative hardnesses between interior and exterior change systematically with exposure age, and cavernous weathering results only on outcrops with long enough exposure ages, on the order of ten to twenty thousand years.

The Towel Creek Tuff in Cottonwood Basin, Arizona, weathers into peculiar forms: conical-shaped tepees which show cavernous weathering as a result of case-hardening by calcite precipitation in the exterior rock. Calcite contents of different materials are observed to vary directly with the abrasion hardness of the material. Basal surfaces are formed at the base of the tepees by heterogeneous fluvial erosion and the cavernous hollows are initiated in these zones. Although infiltration of meteoric water into the tepees occurs through all surfaces, moisture flow during dessication of the tepees occurs primarily through the basal surfaces and the lower cavernous hollows. Equilibrium aqueous chemistry limits the interior rock's carbonate content, but calcite can accumulate at the rock exterior.

Because of the overall differences in the intergranular bonding character between crystalline materials such as granite and clastic materials such as sandstone, the results of this study indicate that crystalline rocks tend to core-soften whereas clastic materials case-harden. Clastic materials will be affected by redistribution of secondary cements and greater accumulation at an interface can result in case hardening. In clastic rocks therefore, the hardness of different areas can either increase or decrease with time. On the other hand, a crystalline rock in a weathering environment will have its intergranular and intragranular bonds disrupted by chemical alteration. Spatial variations in disruption can result in core softening or case softening, but the hardness of all areas will decrease with time. Accumulation of secondary cements can often enhance differential effects in crystalline rocks but without case hardening the rock.

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Book chapters on the topic "Differential weathering"

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Cronan, Christopher S. "Chemical Weathering and Solution Chemistry in Acid Forest Soils: Differential Influence of Soil Type, Biotic Processes, and H+ Deposition." In The Chemistry of Weathering, 175–95. Dordrecht: Springer Netherlands, 1985. http://dx.doi.org/10.1007/978-94-009-5333-8_11.

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Su, Tian-ming, Yan-ge Zhang, Tie-zhu Zhang, and Yi-lin Liu. "Rock Falls in Horizontal Strata Due to Differential Weathering." In Engineering Geology for Society and Territory - Volume 2, 1745–51. Cham: Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-09057-3_309.

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Farley, Kevin J., Geoffrey G. Germann, and Alan W. Elzerman. "Differential Weathering of PCB Congeners in Lake Hartwell, South Carolina." In Advances in Chemistry, 575–600. Washington, DC: American Chemical Society, 1994. http://dx.doi.org/10.1021/ba-1994-0237.ch019.

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"differential weathering." In Dictionary Geotechnical Engineering/Wörterbuch GeoTechnik, 375–76. Berlin, Heidelberg: Springer Berlin Heidelberg, 2014. http://dx.doi.org/10.1007/978-3-642-41714-6_41923.

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Brumm, Adam, Matt Pope, Mathieu Leroyer, and Kate Emery. "Hominin Evolution and Stone Tool Scavenging and Reuse in the Lower Paleolithic." In Squeezing Minds From Stones, 149–78. Oxford University Press, 2019. http://dx.doi.org/10.1093/oso/9780190854614.003.0008.

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This chapter examines evidence for what may be a key stage in the evolution of human cognition: the scavenging and reuse of stone artifacts by Lower Paleolithic hominins, as demonstrated by differential weathering of flake scars, indicating two or more temporally discrete phases of reduction. Such artifacts tend to be uncommon in Lower Paleolithic assemblages; however, an examination of the circumstances under which repatination occurs suggests that the rarity of these objects may underestimate the true scale of tool scavenging and reuse in the remote past. In the chapter the implications are examined, considering a view in which the ability to “read” intent from older stone tools that were still visible in the environment was an integral part of human beings’ evolutionary story.
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Conference papers on the topic "Differential weathering"

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Kutschke, Walter G., William Petersen, and John Meyers. "Rock Slope Protection System for Differential Weathering Materials." In Geo-Denver 2007. Reston, VA: American Society of Civil Engineers, 2007. http://dx.doi.org/10.1061/40905(224)9.

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Su, Tian-ming, and Qiang Sun. "Analysis on differential weathering characters of high cutting slope in Three Gorge Reservoir." In 2011 International Conference on Remote Sensing, Environment and Transportation Engineering (RSETE). IEEE, 2011. http://dx.doi.org/10.1109/rsete.2011.5965077.

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Germanoski, Dru. "DIFFERENTIAL WEATHERING AND RELATIONSHIPS BETWEEN TOPOGRAPHY, LITHOLOGY, AND REGOLITH THICKNESS IN EAST-CENTRAL PENNSYLVANIA." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-306128.

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Davias, Michael, and Thomas H. S. Harris. "AND YET THEY PERSIST; LIDAR BARE-EARTH DEMS ELUCIDATE CAROLINA BAY RIMS AS PALIMPSEST FEATURES CONTROLLING THEIR TOPOGRAPHIC EXPRESSION THROUGH DIFFERENTIAL WEATHERING AND EROSION." In 67th Annual Southeastern GSA Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018se-311644.

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Farid*, Asam, Tanzeel Ur Rehman Sabir, Mahmoud K. Harb, and Rashad Kilani. "Identifying the extent of differential weathering in hard rocks under tank load influence zone, a case study of multichannel analysis of surface waves and seismic refraction." In Fifth International Conference on Engineering Geophysics (ICEG), 21–24 October 2019, Al Ain, UAE. Society of Exploration Geophysicists, 2020. http://dx.doi.org/10.1190/iceg2019-051.1.

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