→ smilenagi:謝謝兩位的分享 01/06 01:48
事實上這兩篇僅在討論地下水分布對土壤性質特別是土壤顏色在空間
上的差異,並沒有真正去討論為何土壤會形成紅色和黃色,其實土壤的紅與黃顏色,
與土壤中鐵氧化物的類型有關,建議可以參考下列文獻:
Schwertmann, U., 1993. Relations between iron oxides, soil color, and
formation. In Bigham, J.M. and Ciolkosz, E.J. (ed.): Soil color, SSSAJ
special publication No. 31. Madison, Wisconsin: Soil Science Society of
America, Inc.
Torrent, J., Schewertman, U., Fechter, H., Alferez, F., 1983. Quantitative
relationships between soil color and hematite content. Soil Science, 136(6):
354-358.
如果要了解台灣洪積母質土壤在不同時間中化育的狀態,可參考下列文獻:
Tsai, H., Huang, W.S., Hseu, Z.Y., Chen, Z.S., 2007. A river terrace
soil chronosequence of the Pakua tableland in central Taiwan. Soil Science,
171(2): 167-179.
뀠引述《Piin (過去 現在與未來)》之銘言：
: Lin, Y (2005)Geomorphology;Soil morphological variations on the Taoyuan Terrace
: Northwestern Taiwan: Roles of topography and groundwater
: Volume 69, Issues 1-4, July 2005, Pages 138-151
: Lin, Y (2007)Geomorphology;Relationships between topography and spatial
: variations in groundwater and soil morphology within the
: Taoyuan-Hukou Tableland, Northwestern Taiwan
: 90 (1-2), pp. 36-54
: 這兩篇說不定對你有點幫助
: 簡之, 在氣候經歷與時間類同的情況下，地下水狀況扮演了非常重要的角色
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