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Geomorphic influences on soil develo...

Gruley, Kristine Emma.

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Geomorphic influences on soil development and soil organic matter dynamics in central Jackson County, Wisconsin.

Record Type:	Electronic resources : Monograph/item
Title/Author:	Geomorphic influences on soil development and soil organic matter dynamics in central Jackson County, Wisconsin./
Author:	Gruley, Kristine Emma.
Description:	157 p.
Notes:	Source: Dissertation Abstracts International, Volume: 76-06(E), Section: A.
Contained By:	Dissertation Abstracts International76-06A(E).
Subject:	Geography. -
Online resource:	http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=3673987
ISBN:	9781321516623

Geomorphic influences on soil development and soil organic matter dynamics in central Jackson County, Wisconsin.
Gruley, Kristine Emma.

Geomorphic influences on soil development and soil organic matter dynamics in central Jackson County, Wisconsin. - 157 p.

Source: Dissertation Abstracts International, Volume: 76-06(E), Section: A.

Thesis (Ph.D.)--The University of Wisconsin - Madison, 2015.

This item must not be sold to any third party vendors.

Sandy and silty mantles in central Jackson County were investigated to characterize, identify, and document past or present geomorphic and pedogenic processes as well as soil organic matter dynamics operational in this landscape. LiDAR, particle size, and silt geochemical data suggest the sand mantle is typically 30 -- 100 cm, no more than 5 m thick, and covers much of the low-relief terrain landscape as a result of widespread eolian activity. The sand mantle acted largely as a surface of transport where saltating sands caused fine-grained material to be re-entrained to be deposited farther downwind. Eolian silt associated with deglaciation is only preserved as silty mantles in the most protected positions along the east and southeast aspects of large bedrock ridges. Silty eolian/colluvial mantles are rich in both coarse and fine silt; whereas, silt found in the sandy mantle in windward locations is dominantly fine silt. Thus, much of the fine silt was likely deposited near the end of widespread eolian activity.

ISBN: 9781321516623Subjects--Topical Terms:

524010
Geography.

Geomorphic influences on soil development and soil organic matter dynamics in central Jackson County, Wisconsin.
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100 1 $a Gruley, Kristine Emma. $3 3172103
245 1 0 $a Geomorphic influences on soil development and soil organic matter dynamics in central Jackson County, Wisconsin.
300 $a 157 p.
500 $a Source: Dissertation Abstracts International, Volume: 76-06(E), Section: A.
500 $a Adviser: Joseph A. Mason.
502 $a Thesis (Ph.D.)--The University of Wisconsin - Madison, 2015.
506 $a This item must not be sold to any third party vendors.
520 $a Sandy and silty mantles in central Jackson County were investigated to characterize, identify, and document past or present geomorphic and pedogenic processes as well as soil organic matter dynamics operational in this landscape. LiDAR, particle size, and silt geochemical data suggest the sand mantle is typically 30 -- 100 cm, no more than 5 m thick, and covers much of the low-relief terrain landscape as a result of widespread eolian activity. The sand mantle acted largely as a surface of transport where saltating sands caused fine-grained material to be re-entrained to be deposited farther downwind. Eolian silt associated with deglaciation is only preserved as silty mantles in the most protected positions along the east and southeast aspects of large bedrock ridges. Silty eolian/colluvial mantles are rich in both coarse and fine silt; whereas, silt found in the sandy mantle in windward locations is dominantly fine silt. Thus, much of the fine silt was likely deposited near the end of widespread eolian activity.
520 $a Without these silty additions, a continuum of podzolization processes would likely dominate the sandy soils based on drainage from Entisols in higher positions to aquic Spodosols in toeslopes. Silty soils have greater inputs of reworked loess are highly acidic and generally unproductive, however, the pedogenic pathway is pushed from podzolization to lessivage. Bisequal soils with an upper E-Bt and lower Ex-Btx are common in these settings. Comparisons of lower sequa characteristics between catena positions suggest lateral flow and translocation through both silty and sandy catenas is an important process in this landscape.
520 $a Soil organic matter (SOM) was compared to fresh organic matter (OM), clay mineralogy and particle size data. SOM in the upper 30 cm show increasing delta 15N and delta13C values and decreasing C:N values with depth, which suggests increased decomposition with depth. In sandy profiles with impeded drainage, podzolization resulted in less decomposed OM protected by organic-mineral complexes with depth. These results point to the importance of understanding the geomorphology and sedimentology of soil parent materials in SOM research as well as the importance of using sampling protocols that are based on horizons rather than incremental depths.
590 $a School code: 0262.
650 4 $a Geography. $3 524010
650 4 $a Agriculture, Soil Science. $3 1017824
650 4 $a Geomorphology. $3 542703
690 $a 0366
690 $a 0481
690 $a 0484
710 2 $a The University of Wisconsin - Madison. $b Geography. $3 3168455
773 0 $t Dissertation Abstracts International $g 76-06A(E).
790 $a 0262
791 $a Ph.D.
792 $a 2015
793 $a English
856 4 0 $u http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=3673987