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    <Identification_Area>
        <logical_identifier>urn:nasa:pds:context:instrument:ksu-hpwel.chepil_wt</logical_identifier>
        <version_id>1.0</version_id>
        <title>Chepil Wind Tunnel at The High Plains Wind Erosion Laboratory, Kansas State University</title>
        <information_model_version>1.11.0.0</information_model_version>
        <product_class>Product_Context</product_class>
        <Modification_History>
            <Modification_Detail>
                <modification_date>2019-02-01</modification_date>
                <version_id>1.0</version_id>
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                 Initial creation of the context product.
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    </Identification_Area>
    <Reference_List>
        <Internal_Reference>
            <lid_reference>urn:nasa:pds:context:facility:laboratory.ksu-hpwel</lid_reference>
            <reference_type>instrument_to_facility</reference_type>
        </Internal_Reference>
        <External_Reference>
            <doi>10.2136/sssaj1959.03615995002300060019x</doi>
            <reference_text>Chepil, W.S. (1959) Equilibrium of Soil Grains at the Threshold of Movement by Wind, Soil Science Society
            of America Journal, 23(6): 422-428.</reference_text>
        </External_Reference>
        <External_Reference>
            <reference_text>Zingg, A. and W.S. Chepil, (1950), Aerodynamics of Wind Erosion, Agr. En., Vol.31, June 1950, pp. 279-282, 284.</reference_text>
        </External_Reference>
    </Reference_List>
    <Instrument>
        <name>Chepil Wind Tunnel at The High Plains Wind Erosion Laboratory, Kansas State University</name>
        <type>Atmospheric Sciences</type>
        <description>
            Historical wind tunnel build by W.S. Chepil at Kansas State University. The tunnel was 17.07 m in length with a cross-section
            area of 0.91 m x 0.91 m, with a boundary layer depth of approximately 0.30 m.
       </description>
    </Instrument>
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