2013-12-1 Impact of the chemo-mineralogical transformations on mechanical properties of iron ore. The chemo-mineralogical reactions described in Section 4.1 correspond to a corrosion of iron ore in a mining environment (presence of H 2 O and O 2) and resulted in its alteration (i.e., chemical weathering). The decrease in material cohesion due to the
ContactRequest PDF On Sep 5, 2013, D. Grgic and others published Impact of chemical weathering on micro/macro-mechanical properties of oolithic iron ore
Contact2021-1-15 The weathering of PE is known to have a strong damaging effect on its chemical and mechanical properties . Physical features like color, shape, surface texture, and other visual characteristics that may contribute to visually distinguishing MPs from other particles, as it was done frequently to separate them from other components of the sample
Contact2016-11-4 Impact of chemical weathering on micro/macro-mechanical properties of oolithic iron ore. Int. J. Rock Mech. Min. Sci., 64 (2013), pp. 236-245. Article Download PDF View Record in Scopus Google Scholar. Gupta and Seshagiri Rao, 2000. A.S. Gupta, K. Seshagiri Rao.
Contact2020-3-1 Therefore, the summary of current weathering data on MPs is helpful for understanding the weathering behavior of macro to micro . 3. Weathering of MPs3.1. Accelerated weathering of MPs. The weathering mechanisms of MPs exhibit similarities with those of macro because of the same molecular compositions (Jahnke et al., 2017). The
ContactRecent weathering studies analyze chemical and morphological changes (Canopoli et al., 2020; Fernández-González et al., 2021; Martínez-Romo et al., 2015;Ojeda et
Contact2017-8-28 This study investigates the effects of weathering on changes in its macroscopic and colour characteristics in connection with changes in its molecular and anatomical structure. Seven hardgoldsuitable for outdoor architecture—bangkirai, cumaru, cumaru rosa, ipé, jatobá, kusia, and massaranduba—were exposed to the exterior out of ground contact for 1–36
Contact2008-11-1 Weathering products and mechanisms of carbonate rocks by microbes were also expounded. The authors put forward four microbial weathering mechanisms of carbonate rocks: (1) microorganisms grow on rock surface or in crevices, resulting in bio-corrosion, bio-erosion, and boring, and accelerate rock decomposition and weathering; (2) boring meshes
Contact2021-11-27 The development of vegetation at ash disposal sites is the only source of organic matter in the substrate through the input of litter and fine roots, i.e. the accumulation of carbon, nitrogen and other essential macro- and micro-elements in the surface layer of FA ponds (Shaw 1992; Zikeli et al. 2002, 2004; Chu 2008; Weber et al. 2015; Pandey
Contact2019-10-29 There are three types of weathering: mechanical, biological, and chemical. Mechanical weathering is caused by wind, sand, rain, freezing, thawing, and other natural forces that can physically alter rock. Biological weathering is caused by the actions of plants and animals as they grow, nest, and burrow. Chemical weathering occurs when rocks
Contact2021-11-27 The development of vegetation at ash disposal sites is the only source of organic matter in the substrate through the input of litter and fine roots, i.e. the accumulation of carbon, nitrogen and other essential macro- and micro-elements in the surface layer of FA ponds (Shaw 1992; Zikeli et al. 2002, 2004; Chu 2008; Weber et al. 2015; Pandey
Contact2021-3-23 The weathering of soil minerals has both long- and short-term consequences for ecosystems. Over the long term soils are denuded as nutrients are leached eventually to oceans. In denuded soils plants must obtain nutrients from conservative cycling or from external inputs to the ecosystem. Over the short-term, mineral weathering can supply nutrients such as K, Ca,
Contact2017-3-14 Chemical weathering of silicate rocks on continents acts as a major sink for atmospheric carbon dioxide and has played an important role in the evolution of the Earth’s climate. However, the
Contact2019-10-29 There are three types of weathering: mechanical, biological, and chemical. Mechanical weathering is caused by wind, sand, rain, freezing, thawing, and other natural forces that can physically alter rock. Biological weathering is caused by the actions of plants and animals as they grow, nest, and burrow. Chemical weathering occurs when rocks
Contact2022-2-9 Bottom ash (BA) is the main residue left by municipal solid waste incineration (MSWI). As the circular economy is strengthened, the use of BA in civil engineering is increasing, but its successful use is hampered by heavy metal leaching. In this study, we investigated the influence of natural weathering (6 months) on the stabilization of heavy metals (Cu, Zn, and Pb) with
Contact2019-12-27 Preparation of water-chemical solution. In real environment, the pH value of underground water is generally 5.5–8.5. However, during waste liquid injection, the
Contact2020-1-22 Both micro- and macro-organisms colonize plastic debris in classical ecological succession from biofilms composed of microorganisms, to complex biofouling communities consisting also of aquatic plants and macrofauna (Fig. 2) (Harrison et al. 2014; Bryant et al. 2016). With smaller particles on the nanometer-centimeter scale, biofilm builds on
Contact2021-5-11 We described in 2017 how weathering plastic litter in the marine environment fulfils two of three criteria to impose a planetary boundary threat related to “chemical pollution and the release of novel entities”: (1) planetary-scale exposure, which (2) is not readily reversible. Whether marine meet the third criterion, (3) eliciting a disruptive impact on vital earth
Contact2022-5-7 resources. Use of natural resources throughout human society leads to many environmental effects such as air and water. pollution, land degradation, and climate changes. Fig. 4. The population
ContactImpacts of increased atmospheric CO2 concentration on photosynthesis and growth of micro- and macro-algae Sci China C Life Sci. 2008 Dec;51(12) :1144-50. in seawater, which alters the carbonate system and related chemical reactions and results in lower pH and higher HCO(3) (-) concentration, affect photosynthetic CO(2) fixation processes of
Contact2017-3-14 Chemical weathering of silicate rocks on continents acts as a major sink for atmospheric carbon dioxide and has played an important role in the evolution of the Earth’s climate. However, the
Contact2021-3-23 The weathering of soil minerals has both long- and short-term consequences for ecosystems. Over the long term soils are denuded as nutrients are leached eventually to oceans. In denuded soils plants must obtain nutrients from conservative cycling or from external inputs to the ecosystem. Over the short-term, mineral weathering can supply nutrients such as K, Ca,
Contact2021-11-27 The development of vegetation at ash disposal sites is the only source of organic matter in the substrate through the input of litter and fine roots, i.e. the accumulation of carbon, nitrogen and other essential macro- and micro-elements in the surface layer of FA ponds (Shaw 1992; Zikeli et al. 2002, 2004; Chu 2008; Weber et al. 2015; Pandey
Contact2022-2-9 Bottom ash (BA) is the main residue left by municipal solid waste incineration (MSWI). As the circular economy is strengthened, the use of BA in civil engineering is increasing, but its successful use is hampered by heavy metal leaching. In this study, we investigated the influence of natural weathering (6 months) on the stabilization of heavy metals (Cu, Zn, and Pb) with
ContactThe weathering process is mainly controlled by mineralogical and chemical composition of the parent rock, climate, and the weathering stage (or age) (Nesbitt and Wilson, 1992; Dontsova et al
ContactImpacts of increased atmospheric CO2 concentration on photosynthesis and growth of micro- and macro-algae Sci China C Life Sci. 2008 Dec;51(12) :1144-50. in seawater, which alters the carbonate system and related chemical reactions and results in lower pH and higher HCO(3) (-) concentration, affect photosynthetic CO(2) fixation processes of
Contact2020-2-13 1. The Plasticene. In the last 70 years, we have abetted an increasing growth in the worldwide production, which has consequently spread into the environment to such a point that we can say to live in a plastic world [1,2].These synthetic polymers are environmental pollutants themselves and act as vectors of transport of various kind of chemicals [], but they
Contact2021-5-11 We described in 2017 how weathering plastic litter in the marine environment fulfils two of three criteria to impose a planetary boundary threat related to “chemical pollution and the release of novel entities”: (1) planetary-scale exposure, which (2) is not readily reversible. Whether marine meet the third criterion, (3) eliciting a disruptive impact on vital earth
Contact2020-1-22 Both micro- and macro-organisms colonize plastic debris in classical ecological succession from biofilms composed of microorganisms, to complex biofouling communities consisting also of aquatic plants and macrofauna (Fig. 2) (Harrison et al. 2014; Bryant et al. 2016). With smaller particles on the nanometer-centimeter scale, biofilm builds on
Contact2015-9-27 2. Chemical weathering process by which the internal structure of a mineral is altered by the addition or removal of elements. Change in phase (mineral type) and composition are due to the action of chemical agents. Chemical weathering is dependent on available surface for reaction temperature and presence of chemically active fluids.
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