Fred J. Young, Ph.D.NRCS Soil Scientist, Columbia, MO
In a typical Missouri county, most if not all separations among soil map units are based on differences in either landform or geology. Recent improvements in Digital Elevation Models (DEM), combined with modeling efforts among many individuals, now allow for GIS modeling of landforms. These landform maps can be combined with geology data to create “geo-landform” units, which are being used to create Ecological Land Types (ELTs) as part of an ecological classification system for Missouri (Nigh et. al, 2000). By adding expert soils knowledge to the geo-landform model (e.g., Zhu et. al, 1997), a soil map model can be produced, which can then be tested and refined by field soil scientists. The final product will be internally consistent, as well as fully integrated with ecological units. Although soil scientists and ecologists have communicated and collaborated, actual soils and ELT mapping has proceeded independently. The objective of the study presented here was to examine the relationship between recent soil survey and ELT mapping for an area in the Missouri Ozarks.
Recent soils mapping was digitized and combined with ELT mapping via GIS (see the Power Point show on the companion CD for details). Crosstabulation tables were derived, showing the percentages of ELT units in each soil map unit, and vice versa. Two soil map units were selected for detailed analysis. Results indicate strong soil-ELT correlations, as well as significant discrepancies. For example, one ELT “shoulder” unit extends down steep convex nose slopes, into areas mapped as backslope soil map units. Other examples are given in the power point show.
In conclusion, explicit integration of soil and ELT units seems possible, but will not become reality unless soil scientists and ecologists work together to define the underlying geo-landform units. For example, where exactly are “shoulder” units located on maps? Can we define ELT and/or soil phases to help integrate these products? I remain cautiously optimistic about such an integration. Soils and ELTs may not match up line-for-line, but hopefully units will “nest”. There may well be ELT criteria that are not relevant to soil survey purposes, and vice versa, and I do not advocate forcing a soil-ELT fit at any cost. However, we in the National Cooperative Soil Survey need to recognize that other natural resource agencies, including the US Forest Service, are committed to using ecological units in their planning (USDA Forest Service, 1993). The more closely we can integrate soils information with these ecological units, the more likely it is that our soils information will be used.
References
Nigh, T.A., C. Becker, J. Grabner, J. Kabrick and D. Meinert. 2000. An ecological classification system for the Current River Hills subsection. Working Draft Manual. Missouri Department of Conservation. Jefferson City, Mo.
USDA Forest Service. 1993. National hierarchical framework of ecological units. Washington, DC: US Department of Agriculture, ECOMAP. 28pp.
Zhu, A, L. Band, R. Vertessey, and B. Dutton. 1997. Derivation of soil properties using a soil land inference model (SoLIM). Soil Sci. Soc. Am. J. 61:523-533.
Carolyn Olson, National Leader- Soil Survey Investigations, NSSC
These materials were compiled from the Investigations Staff and the few researchers who are still located on other staffs.
1. Geographic distribution of research and assistance provided by the Investigations Staff FY 2001. Geophysical assistance was separated out and displayed on a separate map.
2. Topical Research. This list is composed of research activities that the
researchers are currently involved in. It includes joint projects with NCSS
cooperators.
Expert Systems Techniques
Decision Support Tools
Predictive Models
Geophysics
Electromagnetic-Induction Studies (EMI)
Geophysical Program Initiative
Ground-Penetrating-Radar Studies (GPR)
LTER Studies
Involvement in about half of the
24 current LTER sites
Mineralogy and Weathering
Ashy Soils
Deconvolution of XRD
Information
Eolian Admixtures to Tephra
Minerals and Human Health
Nutrient Cycling
Nitrate, Nitrogen
Soil Phosphorus
Pedogenesis
Paralithic Materials and Soil-
Water Properties
Relict Soils and Weathering
Stable Isotopic Studies
Vertisols/Paleovertisols
Salinity in Soils
Irrigation Canal Seepage in Arid
and Semiarid Areas
Scaling of Data and Prediction of Soil
Properties
Bulk Density Studies
Predicting Soil Resistivity
Rock Fragment Conversions
Soil Erosivity Predictions
Use-Dependent and Use-Invariant Data Integration
Soil Biology
Field Sampling Protocol
Methods Development
Microbial Activity and Biomass
Analysis
Soil Carbon
Assessments
Carbon Storage - No till, CRP
Soil Chemistry
Major and Trace Element Studies
Soil Classification
Andisols Properties
Cascade Range Soils
Diagnostic Features
Remotely-sensed inventories
Soil Climate and Hydraulic Properties
of Soils
Hydrologic Indicators
Small-scale Infiltrometer
Comparisons
Soil Color
Soil Hydrology and Water Movement through Landscape
Soil Moisture Studies
Soil Temperature Studies
Soil-Water Regimes
Wet-Soil Monitoring Projects
Soil Geomorphology
Carolina Bays
Chihuahuan Desert Study
Deep Investigations Studies
Mountainous Terrain Models
Macon Ridge
South-central Iowa Terraces
Southern High Plains - MLRA 77
Soil Health
Urban Soils and Anthropogenic
Impacts
3. Announcements:
a. The pending Memorandum of Agreement with State Geological
Surveys and the NRCS.
b. Request for volunteers to take part in the Task Force to develop
regional course curriculum in soil geomorphology.
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