Soil-forming rates and processes on Quaternary moraines near Lago Buenos Aires, Argentina
Soil-forming rates and processes on Quaternary moraines near Lago Buenos Aires, Argentina
复制标题
阿根廷布宜诺斯艾利斯湖附近第四纪冰碛的成土速率和过程
DOI:
10.1016/j.yqres.2005.08.027
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发表时间:
2006
影响因子:
2.3
通讯作者:
Bockheim, James G.
中科院分区:
文献类型:
--
作者:
Douglass, Daniel C.;Bockheim, James G.
Thirty-four pedons on four moraine groups spanning the last 1 myr are used to investigate mechanisms and rates of soil development in Santa Cruz province, Argentina. All soils are coarse-loamy, mesic, Typic Haplocalcids or Calcic Haploxerolls occurring under short grass-shrub steppe, in a semi-arid climate. The dominant soil-forming processes are the accumulation of organic matter, carbonate, and clay-sized particles. Organic carbon accumulates rapidly in these soils, but significantly higher amounts in the oldest two moraine groups are likely the result of slight differences in soil-forming environment or grazing practices. Accumulation rates of carbonate and clay decrease with age, suggesting either decreased influx in the earliest part of the record or attainment of equilibrium between influx and loss. There are no changes in soil redness, and preservation of weatherable minerals in the oldest soils indicates there is little chemical weathering in this environment. Measured dust input explains the accumulation of both clay and carbonate. We present a carbonate cycling model that describes potential sources and calcium mobility in this environment. Calibration of rates of soil formation creates a powerful correlation tool for comparing other glacial deposits in Argentina to the well-dated moraines at Lago Buenos Aires.