Rock type and dust influx control accretionary soil development on hillslopes in the Sandia Mountains, New Mexico, USA

Quaternary Research - Tập 76 - Trang 411-416 - 2011
Lyman P. Persico1, Leslie D. McFadden1, Jedidiah D. Frechette1, Grant A. Meyer1
1The University of New Mexico, Department of Earth and Planetary Sciences, NM, USA

Tóm tắt

Abstract

Lower slopes of the Sandia Mountains are characterized by granitic corestone topography and weathering-limited slopes with thin grusy colluvium and weakly developed soils. In contrast, thick soils with illuvial clay and pedogenic carbonate have developed below aplite outcrops. Aplite is resistant to chemical decomposition, but physically weathers to blocky clasts that enhance surface roughness and erosional resistance of colluvium, promoting accumulation of eolian fines. Thick B horizons on aplite slopes indicate limited erosion and prolonged periods of stability and soil development. Accretion of eolian material limits runoff and prevents attainment of a steady-state balance between soil production and downslope transport.


Tài liệu tham khảo

Muhs, 2007, Loess deposits, origins, and properties, 1405 Pazzaglia, 1999, Phanerozoic geologic evolution of the Albuquerque Area, 97 10.1130/0016-7606(1965)76[1165:STOTSS]2.0.CO;2 10.1016/j.geoderma.2007.01.004 10.1130/0091-7613(1990)018<0549:GAOLQV>2.3.CO;2 10.1130/0091-7613(1987)15<504:IOEAPP>2.0.CO;2 10.1016/0016-7061(70)90055-8 10.1111/j.1365-3091.1995.tb00380.x 10.1016/j.radmeas.2006.04.019 10.1029/1999JD900084 10.1130/0016-7606(2001)113<0305:CTMQAN>2.0.CO;2 10.1016/0016-7037(87)90070-6 10.2475/ajs.267.4.510 10.1130/B26283.1 10.1130/0091-7613(2000)28<787:SPOARE>2.0.CO;2 10.1130/0016-7606(1993)105<1008:RCBDAP>2.3.CO;2 Gilbert, 1880, Report on the Geology of the Henry Mountains, 170 10.1086/627710 Kelley, 1975, Geology of Sandia Mountains and vicinity, New Mexico. New Mexico Bureau of Mines and Mineral Resources, Socorro 10.1029/2008WR007319 Frechette, 2006, Localized lithologic controls on slope forming processes along the Sandia Mountain front. New Mexico Geological Society Spring Meeting, 65 Birkeland, 1999, Soils and Geomorphology 10.1016/S0169-555X(98)00095-6 Gile, 1981, Soils and geomorphology in the basin and range area of Southern New Mexico — guidebook to the desert project. New Mexico Bureau of Mines and Mineral Resources Memoir 39 10.1006/jare.1993.1068 10.1038/41056 Bullock, 1985, Handbook for Soil Thin Section Description Bull, 1991, Geomorphic Responses to Climatic Change 10.1130/0091-7613(2002)030<0195:IOSDOT>2.0.CO;2 10.1130/G23133A.1 10.1016/0033-5894(86)90041-4 Connell, 1999, Pliocene and Quaternary stratigraphy, soils, and geomorphology of the northern flank of the Sandia Mountains, Albuquerque Basin, Rio Grande rift, New Mexico, 379 Gerson, 1987, Rates and modes of dust accretion and deposition in an arid region—the Negev, Israel, 157 10.1038/nature06763 10.1016/S0169-555X(03)00148-X 10.1016/j.yqres.2010.12.002 Eberly, 1996, Eolian dust as a factor in soil development on the Pajarito Plateau, northern New Mexico 10.1086/428808 Porter, 1983, Late Wisconsin mountain glaciation in the western United States, 71 Yair, 2000, Hydrological response of desert margins to climatic change: the effect of changing surface properties, 49 10.1029/2008JF001009 10.1071/SR04158