FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4244175928> ?p ?o ?g. }

• W4244175928 abstract "Abstract. Silicate mineral dissolution rates depend on the interaction of a number of factors categorized either as intrinsic (e.g. mineral surface area, mineral composition) or extrinsic (e.g. climate, hydrology, biological factors, physical weathering). Estimating the integrated effect of these factors on the silicate mineral dissolution rates therefore necessitates the use of fully mechanistic soil evolution models. This study applies a mechanistic soil evolution model (SoilGen) to explore the sensitivity of silicate mineral dissolution rates to the integrated effect of other soil forming processes and factors. The SoilGen soil evolution model is a 1-D model developed to simulate the time-depth evolution of soil properties as a function of various soil forming processes (e.g. water, heat and solute transport, chemical and physical weathering, clay migration, nutrient cycling and bioturbation) driven by soil forming factors (i.e., climate, organisms, relief, parent material). Results from this study show that although soil solution chemistry (pH) plays a dominant role in determining the silicate mineral dissolution rates, all processes that directly or indirectly influence the soil solution composition equally play an important role in driving silicate mineral dissolution rates. Model results demonstrated a decrease of silicate mineral dissolution rates with time, an obvious effect of texture and an indirect but substantial effect of physical weathering on silicate mineral dissolution rates. Results further indicated that clay migration and plant nutrient recycling processes influence the pH and thus the silicate mineral dissolution rates. Our silicate mineral dissolution rates results fall between field and laboratory rates but were rather high and more close to the laboratory rates owing to the assumption of far from equilibrium reaction used in our dissolution rate mechanism. There is therefore need to include secondary mineral precipitation mechanism in our formulation. In addition, there is need for a more detailed study that is specific to field sites with detailed measurements of silicate mineral dissolution rates, climate, hydrology and mineralogy to enable the calibration and validation of the model. Nevertheless, this study is another important step to demonstrate the critical need to couple different soil forming processes with chemical weathering in order to explain differences observed between laboratory and field measured silicate mineral dissolution rates." @default.
• W4244175928 created "2022-05-12" @default.
• W4244175928 creator A5007089168 @default.
• W4244175928 creator A5033355857 @default.
• W4244175928 date "2015-08-26" @default.
• W4244175928 modified "2023-09-27" @default.
• W4244175928 title "Evaluating sensitivity of silicate mineral dissolution rates to physical weathering using a soil evolution model (SoilGen2.25)" @default.
• W4244175928 cites W1509901374 @default.
• W4244175928 cites W1623559396 @default.
• W4244175928 cites W1665574325 @default.
• W4244175928 cites W1749738398 @default.
• W4244175928 cites W1963978415 @default.
• W4244175928 cites W1964575642 @default.
• W4244175928 cites W1967947509 @default.
• W4244175928 cites W1969134186 @default.
• W4244175928 cites W1971178834 @default.
• W4244175928 cites W1972187431 @default.
• W4244175928 cites W1986252155 @default.
• W4244175928 cites W1991620953 @default.
• W4244175928 cites W1993209602 @default.
• W4244175928 cites W1997942048 @default.
• W4244175928 cites W2002348954 @default.
• W4244175928 cites W2003609307 @default.
• W4244175928 cites W2007766503 @default.
• W4244175928 cites W2012330976 @default.
• W4244175928 cites W2012486807 @default.
• W4244175928 cites W2012554282 @default.
• W4244175928 cites W2013756008 @default.
• W4244175928 cites W2014439236 @default.
• W4244175928 cites W2015996529 @default.
• W4244175928 cites W2019280578 @default.
• W4244175928 cites W2022321851 @default.
• W4244175928 cites W2032677315 @default.
• W4244175928 cites W2042208506 @default.
• W4244175928 cites W2046154606 @default.
• W4244175928 cites W2051716726 @default.
• W4244175928 cites W2052276436 @default.
• W4244175928 cites W2053627401 @default.
• W4244175928 cites W2057980421 @default.
• W4244175928 cites W2060587541 @default.
• W4244175928 cites W2060589800 @default.
• W4244175928 cites W2060997333 @default.
• W4244175928 cites W2061097344 @default.
• W4244175928 cites W2061675171 @default.
• W4244175928 cites W2063288995 @default.
• W4244175928 cites W2063635825 @default.
• W4244175928 cites W2064655658 @default.
• W4244175928 cites W2067121254 @default.
• W4244175928 cites W2067228709 @default.
• W4244175928 cites W2068847570 @default.
• W4244175928 cites W2068951595 @default.
• W4244175928 cites W2072205692 @default.
• W4244175928 cites W2076857865 @default.
• W4244175928 cites W2079265495 @default.
• W4244175928 cites W2080756707 @default.
• W4244175928 cites W2085468600 @default.
• W4244175928 cites W2088918302 @default.
• W4244175928 cites W2109261160 @default.
• W4244175928 cites W2113541947 @default.
• W4244175928 cites W2120601523 @default.
• W4244175928 cites W2122771977 @default.
• W4244175928 cites W2124366831 @default.
• W4244175928 cites W2124781550 @default.
• W4244175928 cites W2125893216 @default.
• W4244175928 cites W2143400799 @default.
• W4244175928 cites W2151810991 @default.
• W4244175928 cites W2167044372 @default.
• W4244175928 cites W2332356198 @default.
• W4244175928 cites W2900272251 @default.
• W4244175928 cites W3022563504 @default.
• W4244175928 cites W4299129262 @default.
• W4244175928 cites W999207820 @default.
• W4244175928 doi "https://doi.org/10.5194/bgd-12-13887-2015" @default.
• W4244175928 hasPublicationYear "2015" @default.
• W4244175928 type Work @default.
• W4244175928 citedByCount "0" @default.
• W4244175928 crossrefType "posted-content" @default.
• W4244175928 hasAuthorship W4244175928A5007089168 @default.
• W4244175928 hasAuthorship W4244175928A5033355857 @default.
• W4244175928 hasBestOaLocation W42441759281 @default.
• W4244175928 hasConcept C107872376 @default.
• W4244175928 hasConcept C127313418 @default.
• W4244175928 hasConcept C142796444 @default.
• W4244175928 hasConcept C147789679 @default.
• W4244175928 hasConcept C153389437 @default.
• W4244175928 hasConcept C159390177 @default.
• W4244175928 hasConcept C159750122 @default.
• W4244175928 hasConcept C17409809 @default.
• W4244175928 hasConcept C178790620 @default.
• W4244175928 hasConcept C184269829 @default.
• W4244175928 hasConcept C185592680 @default.
• W4244175928 hasConcept C199289684 @default.
• W4244175928 hasConcept C2776277684 @default.
• W4244175928 hasConcept C2776432453 @default.
• W4244175928 hasConcept C2777335606 @default.
• W4244175928 hasConcept C39432304 @default.
• W4244175928 hasConcept C40212044 @default.
• W4244175928 hasConcept C40724407 @default.
• W4244175928 hasConcept C88380143 @default.
• W4244175928 hasConceptScore W4244175928C107872376 @default.

• next