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• W3090379878 endingPage "114726" @default.
• W3090379878 startingPage "114726" @default.
• W3090379878 abstract "The podzolic soils with characteristic eluvial horizon are widely distributed in the mountainous area of Taiwan with a cold and humid climate, where the altitude is greater than 3000 m above sea level. There are multiple sequence horizons along the soil profile in some of the places. These repeated patterns of the soil horizons have not been reported in the literature, which may indicate the cycles of climatic or environmental changes in the past. The puzzling origin of these soils may be answered by identifying the parent materials and their source areas through age dating and isotopic analyses. Four soil profiles were sampled from Hohuanshan (HHM and HWS), Nanhuashan (NH), and Battonguan (BTG) of the alpine area in central Taiwan. These soils, in general, show the characteristics of silt and silty loam in soil texture, high soil organic carbon, low cation exchange capacity, and low base saturation percentage. Soil classification in accordance with the US System (Soil Taxonomy) suggests all the soils in this study are Humicryepts. The index quantification from soil morphology also shows the extent of pedogenesis fairly between profiles, which is supported by the ages obtained from the charcoals or highly carbonized woods in various sizes found in the dark black soil horizons. It suggests that these soils began to develop approximately four thousand years ago, during the cool and dry period of the Holocene according to the paleoclimate records, and the cold and dry climate favors the preservation of charcoals. Despite the suspicions of aeolian deposits in Taiwan, the high mountain areas are far from the location of aeolian deposits. It was not until recent years that the researchers proposed the idea of aeolian addition to the soils in Hohuanshan. The characteristics of the multiple sequence soil horizons may offer an insight into the paleoenvironment of the high mountain areas. The bimodal pattern on the particle size distribution indicates an additional parental source for these soils. The evidence from the calculated strontium isotope ratios delivers an argument that these soils are developed by in-situ weathering with the addition of aeolian material. They are yellowish and subangular particles with sizes ranging from 7 to 10 µm. The aeolian deposits of Hohuanshan reveal the geochemical characteristics of the river sediments of the Da-An, Da-Chia, Da-Du River, and Cho-Shui Rivers. This suggests that the source of the aeolian particles in the soils was supplied with materials connected with the river system of central Taiwan. In the same manner, the aeolian deposits of Nanhuashan and Battonguan were likely derived from the river sediments of eastern Taiwan. The example from the NH profile indicates a constant rate of aeolian addition, which rules out the influence of the fluctuations of climate change since the mid-Holocene. The findings of this study not only help validate previous studies on the paleoenvironment of Taiwan but also inspire further aspects of the Taiwanese paleoclimate researches." @default.
• W3090379878 created "2020-10-08" @default.
• W3090379878 creator A5013491559 @default.
• W3090379878 creator A5015084951 @default.
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• W3090379878 creator A5052288091 @default.
• W3090379878 creator A5069548112 @default.
• W3090379878 creator A5084477171 @default.
• W3090379878 date "2021-02-01" @default.
• W3090379878 modified "2023-09-27" @default.
• W3090379878 title "Aeolian additions of podzolic soils on the high-altitude mountains in central Taiwan-sediment origin and pedological implications" @default.
• W3090379878 cites W1480605013 @default.
• W3090379878 cites W1557745476 @default.
• W3090379878 cites W1717370574 @default.
• W3090379878 cites W1899286304 @default.
• W3090379878 cites W1964325013 @default.
• W3090379878 cites W1965466615 @default.
• W3090379878 cites W1969763906 @default.
• W3090379878 cites W1969793930 @default.
• W3090379878 cites W1978928936 @default.
• W3090379878 cites W1980189732 @default.
• W3090379878 cites W1986287990 @default.
• W3090379878 cites W1990447751 @default.
• W3090379878 cites W1990625716 @default.
• W3090379878 cites W1991018656 @default.
• W3090379878 cites W1991070819 @default.
• W3090379878 cites W1991491981 @default.
• W3090379878 cites W1994291426 @default.
• W3090379878 cites W1995160959 @default.
• W3090379878 cites W2000198266 @default.
• W3090379878 cites W2001671637 @default.
• W3090379878 cites W2002192561 @default.
• W3090379878 cites W2004724527 @default.
• W3090379878 cites W2007882349 @default.
• W3090379878 cites W2009129310 @default.
• W3090379878 cites W2009243045 @default.
• W3090379878 cites W2010138617 @default.
• W3090379878 cites W2011137266 @default.
• W3090379878 cites W2012045156 @default.
• W3090379878 cites W2018025228 @default.
• W3090379878 cites W2018539923 @default.
• W3090379878 cites W2019300508 @default.
• W3090379878 cites W2020198378 @default.
• W3090379878 cites W2026046835 @default.
• W3090379878 cites W2026678813 @default.
• W3090379878 cites W2027040117 @default.
• W3090379878 cites W2029121471 @default.
• W3090379878 cites W2033189266 @default.
• W3090379878 cites W2038428312 @default.
• W3090379878 cites W2038835052 @default.
• W3090379878 cites W2041621264 @default.
• W3090379878 cites W2044952811 @default.
• W3090379878 cites W2046006545 @default.
• W3090379878 cites W2046240951 @default.
• W3090379878 cites W2052462490 @default.
• W3090379878 cites W2057238843 @default.
• W3090379878 cites W2057870938 @default.
• W3090379878 cites W2071287891 @default.
• W3090379878 cites W2074272256 @default.
• W3090379878 cites W2075921591 @default.
• W3090379878 cites W2081851927 @default.
• W3090379878 cites W2083662941 @default.
• W3090379878 cites W2084378009 @default.
• W3090379878 cites W2084470761 @default.
• W3090379878 cites W2095157870 @default.
• W3090379878 cites W2102029231 @default.
• W3090379878 cites W2113575702 @default.
• W3090379878 cites W2114521266 @default.
• W3090379878 cites W2118495193 @default.
• W3090379878 cites W2119475907 @default.
• W3090379878 cites W2121460345 @default.
• W3090379878 cites W2127209801 @default.
• W3090379878 cites W2132409208 @default.
• W3090379878 cites W2133555891 @default.
• W3090379878 cites W2138049699 @default.
• W3090379878 cites W2140807334 @default.
• W3090379878 cites W2149562083 @default.
• W3090379878 cites W2156856095 @default.
• W3090379878 cites W2163499497 @default.
• W3090379878 cites W2172394941 @default.
• W3090379878 cites W2180637001 @default.
• W3090379878 cites W2212265200 @default.
• W3090379878 cites W2219992834 @default.
• W3090379878 cites W2252343870 @default.
• W3090379878 cites W2341751004 @default.
• W3090379878 cites W2471934652 @default.
• W3090379878 cites W2588853677 @default.
• W3090379878 cites W2593936500 @default.
• W3090379878 cites W2612015931 @default.
• W3090379878 cites W2727623211 @default.
• W3090379878 cites W2766853591 @default.
• W3090379878 cites W2774123728 @default.
• W3090379878 cites W2791625973 @default.
• W3090379878 cites W2795654494 @default.
• W3090379878 cites W2900763852 @default.
• W3090379878 cites W2953413703 @default.
• W3090379878 cites W2959755737 @default.
• W3090379878 cites W2999162121 @default.

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