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<?xml version="1.0"?>
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<eml:eml
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xsi:schemaLocation="eml://ecoinformatics.org/eml-2.0.1 http://sbc.lternet.edu/external/InformationManagement/EML_201schema/eml.xsd"
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packageId="knb-lter-knz.2.4" system="KNB" scope="system"
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xmlns:eml="eml://ecoinformatics.org/eml-2.0.1"
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xmlns:stmml="http://www.xml-cml.org/schema/stmml"
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xmlns:ds="eml://ecoinformatics.org/dataset-2.0.1"
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xmlns:sw="eml://ecoinformatics.org/software-2.0.1"
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xmlns:prot="eml://ecoinformatics.org/protocol-2.0.1"
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xmlns:cit="eml://ecoinformatics.org/literature-2.01"
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xmlns:doc="eml://ecoinformatics.org/documentation-2.0.1"
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xmlns:res="eml://ecoinformatics.org/resource-2.0.1"
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xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance">
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<dataset>
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<alternateIdentifier>AGW01</alternateIdentifier>
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<title>Belowground Water Chemistry from Wells on N04D</title>
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<creator>
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<individualName>
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<givenName>Gwendolyn</givenName>
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<givenName>Lee</givenName>
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<surName>Macpherson</surName>
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</individualName>
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<address>
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<deliveryPoint>120 Lindley Hall, Department of Geology; 1475 Jayhawk Blvd., University of Kansas</deliveryPoint>
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<city>Lawrence</city>
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<administrativeArea>KS</administrativeArea>
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<postalCode>
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</postalCode>
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<country>USA</country>
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</address>
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<phone>785-864-2742</phone>
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<electronicMailAddress>glmac@ku.edu</electronicMailAddress>
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</creator>
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<abstract>
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<section>
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<para>In 1988 and 1990, the U.S. Geological Survey, Lawrence, KS, drilled 35 wells at 16
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sites within the N04D watershed at the Konza Prairie Research Natural Area. The wells
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range in depth from about 2 to 13 meters, and are nested to include wells completed in
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alluvium/colluvium near the N04D drainage and in two Permian-aged limestoneâs. These sites
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comprise four transects running approximately east-west across the drainage, and occupy
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the lower 10% of the surface area of the watershed. The geology of the area is
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characterized by patchy, near-stream alluvium/colluvium which overlies bedrock, composed
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of thin (1-2 meter) limestones alternating with thicker (2-4 meter) shales. The limestones
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are fractured, and records of water levels in the wells show that in some parts of the
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watershed water levels are nearly constant, while in others they respond noticeably to
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precipitation events. Beginning in 1991, water samples for inorganic chemical analysis
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have been collected every four to six weeks by bailing wells to remove 1-2 well volumes. A
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bailed sample is then filtered through 0.45µ membrane filters by gravity feed. One 50-mL
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aliquot is reserved for alkalinity determination by titration with 0.02 N H2SO4. One
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250-mL LDPE bottle is filled with 250 mL of sample and 5 mL of concentrated HNO3 for
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cation analysis by atomic absorption spectrophotometry (Na, K, Ca, Mg). One 250-mL LDPE
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bottle is filled to the brim for anion analysis by ion chromatography (Cl, SO4, NO3). The
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latter two samples are stored on ice and later in a refrigerator. Anion determination is
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completed within 1 to 3 days of collection.</para>
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</section>
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</abstract>
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<keywordSet>
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<keyword>Ca</keyword>
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<keyword>chemical hydrogeology</keyword>
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<keyword>chemistry</keyword>
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<keyword>inorganic ground-water chemistry</keyword>
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<keyword>low-temperature aqueous geochemistry</keyword>
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<keyword>organic</keyword>
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<keyword>subsurface water chemistry</keyword>
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<keyword>temperature</keyword>
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<keyword>water</keyword>
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</keywordSet>
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<distribution>
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<online>
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<url>http://www.konza.ksu.edu/harvest/PASTA/AGW011.CSV</url>
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</online>
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</distribution>
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<coverage>
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<temporalCoverage>
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<rangeOfDates>
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<beginDate>
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<calendarDate>1991-01-19</calendarDate>
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</beginDate>
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<endDate>
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<calendarDate> 2050-01-01 </calendarDate>
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</endDate>
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</rangeOfDates>
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</temporalCoverage>
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</coverage>
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<contact id="im">
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<positionName>KNZ-LTER Data Manager</positionName>
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<address>
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<deliveryPoint> Division of Biology</deliveryPoint>
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<deliveryPoint> Kansas State University</deliveryPoint>
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<city>Manhattan</city>
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<administrativeArea>KS</administrativeArea>
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<postalCode>66506</postalCode>
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</address>
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<phone phonetype="voice">(785)532-6729</phone>
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<phone phonetype="fax">(785)532-6653</phone>
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<electronicMailAddress>knzlter@ksu.edu</electronicMailAddress>
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<onlineUrl>http://www.konza.ksu.edu</onlineUrl>
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</contact>
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<methods>
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<methodStep>
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<description>
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<para>
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<literalLayout> Method manual is available at http://www.konza.ksu.edu <Long
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Text></literalLayout>
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</para>
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</description>
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</methodStep>
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</methods>
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<access authSystem="knb" order="allowFirst" scope="document">
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<allow>
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<principal>uid=KNZ,o=lter,dc=ecoinformatics,dc=org</principal>
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<permission>all</permission>
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</allow>
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<allow>
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<principal>public</principal>
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<permission>read</permission>
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</allow>
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</access>
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<dataTable>
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<alternateIdentifier>AGW011</alternateIdentifier>
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<entityName> </entityName>
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<entityDescription>CODES USED: ow-observation well; 1-4: Transects(1-4), the lowest number in
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nearest the concrete weir; 1-6: Number unique to the well site (1 is nearest from the
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stream; 3 is fathest from the stream on the east or northeast side. Well site number 4-6 are
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progressively further away from the stream on the west or southwest side of the stream.
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Alpha chara: Eis=Eiss Limestone, Eis1=Lower Eiss Limestone, Eis2=Upper Eiss Limestone,
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Mor=Morril Limestone, Al = Alluvium-colluvium. Other notes: '-1' means concentration was
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below detection limit of instrument or method used; 'null' means not analyzed or not
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appropriate (as in water level elevation is not appropriate variable for stream samples) or
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not available (no sample taken or laboratory error).</entityDescription>
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<coverage>
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<temporalCoverage>
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<rangeOfDates>
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<beginDate>
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<calendarDate>1990-01-01</calendarDate>
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</beginDate>
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<endDate>
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<calendarDate> 2050-01-01 </calendarDate>
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</endDate>
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</rangeOfDates>
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</temporalCoverage>
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</coverage>
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<attributeList>
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<attribute>
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<attributeName>ID</attributeName>
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<attributeDefinition> </attributeDefinition>
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<storageType>int</storageType>
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<measurementScale>
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<interval>
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<unit>
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<standardUnit>dimensionless</standardUnit>
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</unit>
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<precision>1</precision>
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<numericDomain>
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<numberType>natural</numberType>
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</numericDomain>
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</interval>
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</measurementScale>
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</attribute>
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<attribute>
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<attributeName>datacode</attributeName>
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<attributeDefinition>Dataset code</attributeDefinition>
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<storageType>char(5)</storageType>
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<measurementScale>
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<nominal>
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<nonNumericDomain>
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<textDomain>
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<definition>Dataset code</definition>
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</textDomain>
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</nonNumericDomain>
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</nominal>
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</measurementScale>
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</attribute>
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<attribute>
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<attributeName>rectype</attributeName>
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<attributeDefinition> </attributeDefinition>
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<storageType>smallint</storageType>
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<measurementScale>
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<interval>
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<unit>
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<standardUnit>dimensionless</standardUnit>
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</unit>
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<precision>1</precision>
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<numericDomain>
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<numberType>natural</numberType>
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</numericDomain>
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</interval>
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</measurementScale>
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</attribute>
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<attribute>
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<attributeName>Transect#</attributeName>
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<attributeDefinition>Number of transects</attributeDefinition>
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<storageType>int</storageType>
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<measurementScale>
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<ratio>
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<unit>
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<standardUnit>dimensionless</standardUnit>
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</unit>
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<precision>1</precision>
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<numericDomain>
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<numberType>natural</numberType>
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</numericDomain>
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</ratio>
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</measurementScale>
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</attribute>
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<attribute>
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<attributeName>Plot#</attributeName>
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<attributeDefinition>Number of plots</attributeDefinition>
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<storageType>int</storageType>
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<measurementScale>
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<ratio>
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<unit>
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<standardUnit>dimensionless</standardUnit>
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</unit>
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<precision>1</precision>
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<numericDomain>
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<numberType>natural</numberType>
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</numericDomain>
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</ratio>
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</measurementScale>
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</attribute>
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<attribute>
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<attributeName>Geology</attributeName>
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<attributeDefinition>Name of geology formation</attributeDefinition>
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<storageType>char(8)</storageType>
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<measurementScale>
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<nominal>
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<nonNumericDomain>
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<textDomain>
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<definition>Name of geology formation</definition>
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</textDomain>
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</nonNumericDomain>
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</nominal>
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</measurementScale>
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</attribute>
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<attribute>
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<attributeName>Date1</attributeName>
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<attributeDefinition>Date water level was measured</attributeDefinition>
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<storageType>datetime</storageType>
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<measurementScale>
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<datetime>
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<formatString>number</formatString>
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<dateTimePrecision>1</dateTimePrecision>
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<dateTimeDomain>
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<bounds>
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<minimum exclusive="false"> </minimum>
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<maximum exclusive="false"> </maximum>
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</bounds>
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</dateTimeDomain>
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</datetime>
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</measurementScale>
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</attribute>
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<attribute>
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<attributeName>Elevation</attributeName>
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<attributeDefinition>Water level elevation above mean sea level</attributeDefinition>
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<storageType>numeric(5,2)</storageType>
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<measurementScale>
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<ratio>
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<unit>
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<standardUnit>dimensionless</standardUnit>
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</unit>
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<precision>0.01</precision>
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<numericDomain>
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<numberType>real</numberType>
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</numericDomain>
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</ratio>
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</measurementScale>
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</attribute>
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<attribute>
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<attributeName>Na1</attributeName>
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<attributeDefinition>Sodium oncentration in milligram per liter,determined by atomic
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absorption spectrometry or ion chromatography</attributeDefinition>
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<storageType>numeric(5,2)</storageType>
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<measurementScale>
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<ratio>
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<unit>
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<standardUnit>dimensionless</standardUnit>
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</unit>
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<precision>0.01</precision>
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<numericDomain>
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<numberType>real</numberType>
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</numericDomain>
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</ratio>
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</measurementScale>
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</attribute>
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<attribute>
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<attributeName>Na2</attributeName>
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<attributeDefinition>Sodium concentration in parts per million, determined by
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inductively-coupled plasma optical emission spectrometry</attributeDefinition>
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<storageType>numeric(5,2)</storageType>
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<measurementScale>
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<ratio>
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<unit>
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<standardUnit>dimensionless</standardUnit>
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</unit>
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<precision>0.01</precision>
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<numericDomain>
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<numberType>real</numberType>
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</numericDomain>
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</ratio>
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</measurementScale>
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</attribute>
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<attribute>
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<attributeName>K1</attributeName>
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<attributeDefinition>Potassium concentration in milligram per liter,determined by atomic
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absorption spectrometry or ion chromatography</attributeDefinition>
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<storageType>numeric(5,2)</storageType>
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<measurementScale>
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<ratio>
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<unit>
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<standardUnit>dimensionless</standardUnit>
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</unit>
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<precision>0.01</precision>
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<numericDomain>
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<numberType>real</numberType>
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</numericDomain>
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</ratio>
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</measurementScale>
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</attribute>
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<attribute>
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<attributeName>K2</attributeName>
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<attributeDefinition>Potassium concentration in in parts per million ,determined by
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inductively-coupled plasma optical emission</attributeDefinition>
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<storageType>numeric(5,2)</storageType>
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<measurementScale>
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<ratio>
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<unit>
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<standardUnit>dimensionless</standardUnit>
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</unit>
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<precision>0.01</precision>
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<numericDomain>
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<numberType>real</numberType>
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</numericDomain>
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</ratio>
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</measurementScale>
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</attribute>
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<attribute>
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<attributeName>Li</attributeName>
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<attributeDefinition>Lithium concentration in parts per million ,determined by
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inductively-coupled plasma optical emission</attributeDefinition>
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<storageType>numeric(5,2)</storageType>
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<measurementScale>
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<ratio>
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<unit>
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<standardUnit>dimensionless</standardUnit>
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</unit>
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<precision>0.01</precision>
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<numericDomain>
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<numberType>real</numberType>
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</numericDomain>
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</ratio>
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</measurementScale>
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</attribute>
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<attribute>
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<attributeName>NH4-N</attributeName>
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<attributeDefinition>Ammonium concentration in milligram nitrogen (N) per liter,
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determined by ion chromatography</attributeDefinition>
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<storageType>numeric(5,2)</storageType>
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<measurementScale>
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<ratio>
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<unit>
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<standardUnit>dimensionless</standardUnit>
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</unit>
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<precision>0.01</precision>
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<numericDomain>
|
|
366
|
<numberType>real</numberType>
|
|
367
|
</numericDomain>
|
|
368
|
</ratio>
|
|
369
|
</measurementScale>
|
|
370
|
</attribute>
|
|
371
|
<attribute>
|
|
372
|
<attributeName>Ca1</attributeName>
|
|
373
|
<attributeDefinition>Calcium concentration in milligram per liter, determined by atomic
|
|
374
|
absorption spectrometry or ion chromatography</attributeDefinition>
|
|
375
|
<storageType>numeric(5,2)</storageType>
|
|
376
|
<measurementScale>
|
|
377
|
<ratio>
|
|
378
|
<unit>
|
|
379
|
<standardUnit>dimensionless</standardUnit>
|
|
380
|
</unit>
|
|
381
|
<precision>0.01</precision>
|
|
382
|
<numericDomain>
|
|
383
|
<numberType>real</numberType>
|
|
384
|
</numericDomain>
|
|
385
|
</ratio>
|
|
386
|
</measurementScale>
|
|
387
|
</attribute>
|
|
388
|
<attribute>
|
|
389
|
<attributeName>Ca2</attributeName>
|
|
390
|
<attributeDefinition>Calcium concentration in parts per million, determined by
|
|
391
|
inductively-coupled plasma optical emission spectrometry</attributeDefinition>
|
|
392
|
<storageType>numeric(5,2)</storageType>
|
|
393
|
<measurementScale>
|
|
394
|
<ratio>
|
|
395
|
<unit>
|
|
396
|
<standardUnit>dimensionless</standardUnit>
|
|
397
|
</unit>
|
|
398
|
<precision>0.01</precision>
|
|
399
|
<numericDomain>
|
|
400
|
<numberType>real</numberType>
|
|
401
|
</numericDomain>
|
|
402
|
</ratio>
|
|
403
|
</measurementScale>
|
|
404
|
</attribute>
|
|
405
|
<attribute>
|
|
406
|
<attributeName>Mg1</attributeName>
|
|
407
|
<attributeDefinition>Magnesium concentration in milligram per liter, determined by atomic
|
|
408
|
absorption spectrometry or ion chromatography</attributeDefinition>
|
|
409
|
<storageType>numeric(5,2)</storageType>
|
|
410
|
<measurementScale>
|
|
411
|
<ratio>
|
|
412
|
<unit>
|
|
413
|
<standardUnit>dimensionless</standardUnit>
|
|
414
|
</unit>
|
|
415
|
<precision>0.01</precision>
|
|
416
|
<numericDomain>
|
|
417
|
<numberType>real</numberType>
|
|
418
|
</numericDomain>
|
|
419
|
</ratio>
|
|
420
|
</measurementScale>
|
|
421
|
</attribute>
|
|
422
|
<attribute>
|
|
423
|
<attributeName>Mg2</attributeName>
|
|
424
|
<attributeDefinition>Magnesium concentration in parts per million, determined by
|
|
425
|
inductively-coupled plasma optical emission spectrometry</attributeDefinition>
|
|
426
|
<storageType>numeric(5,2)</storageType>
|
|
427
|
<measurementScale>
|
|
428
|
<ratio>
|
|
429
|
<unit>
|
|
430
|
<standardUnit>dimensionless</standardUnit>
|
|
431
|
</unit>
|
|
432
|
<precision>0.01</precision>
|
|
433
|
<numericDomain>
|
|
434
|
<numberType>real</numberType>
|
|
435
|
</numericDomain>
|
|
436
|
</ratio>
|
|
437
|
</measurementScale>
|
|
438
|
</attribute>
|
|
439
|
<attribute>
|
|
440
|
<attributeName>Sr</attributeName>
|
|
441
|
<attributeDefinition>Strontium concentration in parts per million, determined by
|
|
442
|
inductively-coupled plasma optical emission spectrometry</attributeDefinition>
|
|
443
|
<storageType>numeric(5,2)</storageType>
|
|
444
|
<measurementScale>
|
|
445
|
<ratio>
|
|
446
|
<unit>
|
|
447
|
<standardUnit>dimensionless</standardUnit>
|
|
448
|
</unit>
|
|
449
|
<precision>0.01</precision>
|
|
450
|
<numericDomain>
|
|
451
|
<numberType>real</numberType>
|
|
452
|
</numericDomain>
|
|
453
|
</ratio>
|
|
454
|
</measurementScale>
|
|
455
|
</attribute>
|
|
456
|
<attribute>
|
|
457
|
<attributeName>Ba</attributeName>
|
|
458
|
<attributeDefinition>Barium concentration in parts per million, determined by
|
|
459
|
inductively-coupled plasma optical emission spectrometry</attributeDefinition>
|
|
460
|
<storageType>numeric(5,2)</storageType>
|
|
461
|
<measurementScale>
|
|
462
|
<ratio>
|
|
463
|
<unit>
|
|
464
|
<standardUnit>dimensionless</standardUnit>
|
|
465
|
</unit>
|
|
466
|
<precision>0.01</precision>
|
|
467
|
<numericDomain>
|
|
468
|
<numberType>real</numberType>
|
|
469
|
</numericDomain>
|
|
470
|
</ratio>
|
|
471
|
</measurementScale>
|
|
472
|
</attribute>
|
|
473
|
<attribute>
|
|
474
|
<attributeName>SO4</attributeName>
|
|
475
|
<attributeDefinition>Soncentration in parts per million, determined by ion
|
|
476
|
chromatography</attributeDefinition>
|
|
477
|
<storageType>numeric(5,2)</storageType>
|
|
478
|
<measurementScale>
|
|
479
|
<ratio>
|
|
480
|
<unit>
|
|
481
|
<standardUnit>dimensionless</standardUnit>
|
|
482
|
</unit>
|
|
483
|
<precision>0.01</precision>
|
|
484
|
<numericDomain>
|
|
485
|
<numberType>real</numberType>
|
|
486
|
</numericDomain>
|
|
487
|
</ratio>
|
|
488
|
</measurementScale>
|
|
489
|
</attribute>
|
|
490
|
<attribute>
|
|
491
|
<attributeName>F</attributeName>
|
|
492
|
<attributeDefinition>Fluoride concentration in parts per million, determined by ion
|
|
493
|
chromatography</attributeDefinition>
|
|
494
|
<storageType>numeric(5,2)</storageType>
|
|
495
|
<measurementScale>
|
|
496
|
<ratio>
|
|
497
|
<unit>
|
|
498
|
<standardUnit>dimensionless</standardUnit>
|
|
499
|
</unit>
|
|
500
|
<precision>0.01</precision>
|
|
501
|
<numericDomain>
|
|
502
|
<numberType>real</numberType>
|
|
503
|
</numericDomain>
|
|
504
|
</ratio>
|
|
505
|
</measurementScale>
|
|
506
|
</attribute>
|
|
507
|
<attribute>
|
|
508
|
<attributeName>Cl</attributeName>
|
|
509
|
<attributeDefinition>Chloride concentration in parts per million, determined by ion
|
|
510
|
chromatography</attributeDefinition>
|
|
511
|
<storageType>numeric(5,2)</storageType>
|
|
512
|
<measurementScale>
|
|
513
|
<ratio>
|
|
514
|
<unit>
|
|
515
|
<standardUnit>dimensionless</standardUnit>
|
|
516
|
</unit>
|
|
517
|
<precision>0.01</precision>
|
|
518
|
<numericDomain>
|
|
519
|
<numberType>real</numberType>
|
|
520
|
</numericDomain>
|
|
521
|
</ratio>
|
|
522
|
</measurementScale>
|
|
523
|
</attribute>
|
|
524
|
<attribute>
|
|
525
|
<attributeName>NO3-N</attributeName>
|
|
526
|
<attributeDefinition>Nitrate concentration in parts per million as nitrogen (N),
|
|
527
|
determined by ion chromatography</attributeDefinition>
|
|
528
|
<storageType>numeric(5,2)</storageType>
|
|
529
|
<measurementScale>
|
|
530
|
<ratio>
|
|
531
|
<unit>
|
|
532
|
<standardUnit>dimensionless</standardUnit>
|
|
533
|
</unit>
|
|
534
|
<precision>0.01</precision>
|
|
535
|
<numericDomain>
|
|
536
|
<numberType>real</numberType>
|
|
537
|
</numericDomain>
|
|
538
|
</ratio>
|
|
539
|
</measurementScale>
|
|
540
|
</attribute>
|
|
541
|
<attribute>
|
|
542
|
<attributeName>HPO4-P</attributeName>
|
|
543
|
<attributeDefinition>Phosphate concentration in parts per million phosphorous (P),
|
|
544
|
determined by ion chromatography</attributeDefinition>
|
|
545
|
<storageType>numeric(5,2)</storageType>
|
|
546
|
<measurementScale>
|
|
547
|
<ratio>
|
|
548
|
<unit>
|
|
549
|
<standardUnit>dimensionless</standardUnit>
|
|
550
|
</unit>
|
|
551
|
<precision>0.01</precision>
|
|
552
|
<numericDomain>
|
|
553
|
<numberType>real</numberType>
|
|
554
|
</numericDomain>
|
|
555
|
</ratio>
|
|
556
|
</measurementScale>
|
|
557
|
</attribute>
|
|
558
|
<attribute>
|
|
559
|
<attributeName>Alkalinity</attributeName>
|
|
560
|
<attributeDefinition>Titration alkalinity (as HCO3) reported as parts per million
|
|
561
|
bicarbonate</attributeDefinition>
|
|
562
|
<storageType>numeric(5,2)</storageType>
|
|
563
|
<measurementScale>
|
|
564
|
<ratio>
|
|
565
|
<unit>
|
|
566
|
<standardUnit>dimensionless</standardUnit>
|
|
567
|
</unit>
|
|
568
|
<precision>0.01</precision>
|
|
569
|
<numericDomain>
|
|
570
|
<numberType>real</numberType>
|
|
571
|
</numericDomain>
|
|
572
|
</ratio>
|
|
573
|
</measurementScale>
|
|
574
|
</attribute>
|
|
575
|
<attribute>
|
|
576
|
<attributeName>pH1</attributeName>
|
|
577
|
<attributeDefinition>Deliberate degassing bottle pH at 13°C (lab pH)</attributeDefinition>
|
|
578
|
<storageType>numeric(5,2)</storageType>
|
|
579
|
<measurementScale>
|
|
580
|
<ratio>
|
|
581
|
<unit>
|
|
582
|
<standardUnit>dimensionless</standardUnit>
|
|
583
|
</unit>
|
|
584
|
<precision>0.01</precision>
|
|
585
|
<numericDomain>
|
|
586
|
<numberType>real</numberType>
|
|
587
|
</numericDomain>
|
|
588
|
</ratio>
|
|
589
|
</measurementScale>
|
|
590
|
</attribute>
|
|
591
|
<attribute>
|
|
592
|
<attributeName>pH2</attributeName>
|
|
593
|
<attributeDefinition>pH measured on site in the field</attributeDefinition>
|
|
594
|
<storageType>numeric(5,2)</storageType>
|
|
595
|
<measurementScale>
|
|
596
|
<ratio>
|
|
597
|
<unit>
|
|
598
|
<standardUnit>dimensionless</standardUnit>
|
|
599
|
</unit>
|
|
600
|
<precision>0.01</precision>
|
|
601
|
<numericDomain>
|
|
602
|
<numberType>real</numberType>
|
|
603
|
</numericDomain>
|
|
604
|
</ratio>
|
|
605
|
</measurementScale>
|
|
606
|
</attribute>
|
|
607
|
<attribute>
|
|
608
|
<attributeName>T</attributeName>
|
|
609
|
<attributeDefinition>Temperature of water at time of field pH
|
|
610
|
measurement</attributeDefinition>
|
|
611
|
<storageType>numeric(5,2)</storageType>
|
|
612
|
<measurementScale>
|
|
613
|
<ratio>
|
|
614
|
<unit>
|
|
615
|
<standardUnit>dimensionless</standardUnit>
|
|
616
|
</unit>
|
|
617
|
<precision>0.01</precision>
|
|
618
|
<numericDomain>
|
|
619
|
<numberType>real</numberType>
|
|
620
|
</numericDomain>
|
|
621
|
</ratio>
|
|
622
|
</measurementScale>
|
|
623
|
</attribute>
|
|
624
|
<attribute>
|
|
625
|
<attributeName>Si1</attributeName>
|
|
626
|
<attributeDefinition>Orthosilicic acid concentration reported as milligrams silica (Si)
|
|
627
|
per liter, determined by the molybdosilicate method with a spectrophotometer at
|
|
628
|
wavelength 410 nm</attributeDefinition>
|
|
629
|
<storageType>numeric(5,2)</storageType>
|
|
630
|
<measurementScale>
|
|
631
|
<ratio>
|
|
632
|
<unit>
|
|
633
|
<standardUnit>dimensionless</standardUnit>
|
|
634
|
</unit>
|
|
635
|
<precision>0.01</precision>
|
|
636
|
<numericDomain>
|
|
637
|
<numberType>real</numberType>
|
|
638
|
</numericDomain>
|
|
639
|
</ratio>
|
|
640
|
</measurementScale>
|
|
641
|
</attribute>
|
|
642
|
<attribute>
|
|
643
|
<attributeName>Si2</attributeName>
|
|
644
|
<attributeDefinition>Orthosilicic acid concentration reported as parts per million as
|
|
645
|
silica (Si), determined by inductively-coupled plasma optical emission
|
|
646
|
spectrometry</attributeDefinition>
|
|
647
|
<storageType>numeric(5,2)</storageType>
|
|
648
|
<measurementScale>
|
|
649
|
<ratio>
|
|
650
|
<unit>
|
|
651
|
<standardUnit>dimensionless</standardUnit>
|
|
652
|
</unit>
|
|
653
|
<precision>0.01</precision>
|
|
654
|
<numericDomain>
|
|
655
|
<numberType>real</numberType>
|
|
656
|
</numericDomain>
|
|
657
|
</ratio>
|
|
658
|
</measurementScale>
|
|
659
|
</attribute>
|
|
660
|
<attribute>
|
|
661
|
<attributeName>B</attributeName>
|
|
662
|
<attributeDefinition>Boron (total) concentration reported as parts per million boron (B),
|
|
663
|
determined by inductively-coupled plasma optical emission
|
|
664
|
spectrometry</attributeDefinition>
|
|
665
|
<storageType>numeric(5,2)</storageType>
|
|
666
|
<measurementScale>
|
|
667
|
<ratio>
|
|
668
|
<unit>
|
|
669
|
<standardUnit>dimensionless</standardUnit>
|
|
670
|
</unit>
|
|
671
|
<precision>0.01</precision>
|
|
672
|
<numericDomain>
|
|
673
|
<numberType>real</numberType>
|
|
674
|
</numericDomain>
|
|
675
|
</ratio>
|
|
676
|
</measurementScale>
|
|
677
|
</attribute>
|
|
678
|
<attribute>
|
|
679
|
<attributeName>Conduct</attributeName>
|
|
680
|
<attributeDefinition>Specific conductance, µS/cm, determined using an Orion model 126
|
|
681
|
4-electrode conductivity cell or Fisher Accumet AR20 2-cell conductivity cell, or
|
|
682
|
equivalent, and reported in microSiemens per centimeter at 20°C</attributeDefinition>
|
|
683
|
<storageType>numeric(5,2)</storageType>
|
|
684
|
<measurementScale>
|
|
685
|
<ratio>
|
|
686
|
<unit>
|
|
687
|
<standardUnit>dimensionless</standardUnit>
|
|
688
|
</unit>
|
|
689
|
<precision>0.01</precision>
|
|
690
|
<numericDomain>
|
|
691
|
<numberType>real</numberType>
|
|
692
|
</numericDomain>
|
|
693
|
</ratio>
|
|
694
|
</measurementScale>
|
|
695
|
</attribute>
|
|
696
|
</attributeList>
|
|
697
|
</dataTable>
|
|
698
|
<dataTable>
|
|
699
|
<alternateIdentifier>AGW012</alternateIdentifier>
|
|
700
|
<entityName> </entityName>
|
|
701
|
<entityDescription>Geographic information of wells for Konza underground water chemical
|
|
702
|
analysis</entityDescription>
|
|
703
|
<coverage>
|
|
704
|
<temporalCoverage>
|
|
705
|
<rangeOfDates>
|
|
706
|
<beginDate>
|
|
707
|
<calendarDate>1990-01-01</calendarDate>
|
|
708
|
</beginDate>
|
|
709
|
<endDate>
|
|
710
|
<calendarDate> 2050-01-01 </calendarDate>
|
|
711
|
</endDate>
|
|
712
|
</rangeOfDates>
|
|
713
|
</temporalCoverage>
|
|
714
|
</coverage>
|
|
715
|
<attributeList>
|
|
716
|
<attribute>
|
|
717
|
<attributeName>Trans#</attributeName>
|
|
718
|
<attributeDefinition>Transect identity</attributeDefinition>
|
|
719
|
<storageType>int</storageType>
|
|
720
|
<measurementScale>
|
|
721
|
<ratio>
|
|
722
|
<unit>
|
|
723
|
<standardUnit>dimensionless</standardUnit>
|
|
724
|
</unit>
|
|
725
|
<precision>1</precision>
|
|
726
|
<numericDomain>
|
|
727
|
<numberType>natural</numberType>
|
|
728
|
</numericDomain>
|
|
729
|
</ratio>
|
|
730
|
</measurementScale>
|
|
731
|
</attribute>
|
|
732
|
<attribute>
|
|
733
|
<attributeName>PlotID</attributeName>
|
|
734
|
<attributeDefinition>Plot identity</attributeDefinition>
|
|
735
|
<storageType>int</storageType>
|
|
736
|
<measurementScale>
|
|
737
|
<ratio>
|
|
738
|
<unit>
|
|
739
|
<standardUnit>dimensionless</standardUnit>
|
|
740
|
</unit>
|
|
741
|
<precision>1</precision>
|
|
742
|
<numericDomain>
|
|
743
|
<numberType>natural</numberType>
|
|
744
|
</numericDomain>
|
|
745
|
</ratio>
|
|
746
|
</measurementScale>
|
|
747
|
</attribute>
|
|
748
|
<attribute>
|
|
749
|
<attributeName>Abname</attributeName>
|
|
750
|
<attributeDefinition>Abriage name of geology formation</attributeDefinition>
|
|
751
|
<storageType>char(8)</storageType>
|
|
752
|
<measurementScale>
|
|
753
|
<nominal>
|
|
754
|
<nonNumericDomain>
|
|
755
|
<textDomain>
|
|
756
|
<definition>Abriage name of geology formation</definition>
|
|
757
|
</textDomain>
|
|
758
|
</nonNumericDomain>
|
|
759
|
</nominal>
|
|
760
|
</measurementScale>
|
|
761
|
</attribute>
|
|
762
|
<attribute>
|
|
763
|
<attributeName>FullName</attributeName>
|
|
764
|
<attributeDefinition>Full name of geology formation</attributeDefinition>
|
|
765
|
<storageType>nvarchar(255)</storageType>
|
|
766
|
<measurementScale>
|
|
767
|
<nominal>
|
|
768
|
<nonNumericDomain>
|
|
769
|
<textDomain>
|
|
770
|
<definition>Full name of geology formation</definition>
|
|
771
|
</textDomain>
|
|
772
|
</nonNumericDomain>
|
|
773
|
</nominal>
|
|
774
|
</measurementScale>
|
|
775
|
</attribute>
|
|
776
|
<attribute>
|
|
777
|
<attributeName>Elevation</attributeName>
|
|
778
|
<attributeDefinition>Elevation of wells above see level</attributeDefinition>
|
|
779
|
<storageType>numeric(5,2)</storageType>
|
|
780
|
<measurementScale>
|
|
781
|
<ratio>
|
|
782
|
<unit>
|
|
783
|
<standardUnit>dimensionless</standardUnit>
|
|
784
|
</unit>
|
|
785
|
<precision>0.01</precision>
|
|
786
|
<numericDomain>
|
|
787
|
<numberType>real</numberType>
|
|
788
|
</numericDomain>
|
|
789
|
</ratio>
|
|
790
|
</measurementScale>
|
|
791
|
</attribute>
|
|
792
|
<attribute>
|
|
793
|
<attributeName>Latitude</attributeName>
|
|
794
|
<attributeDefinition>Latitude in geographic projection (decimal
|
|
795
|
degree)</attributeDefinition>
|
|
796
|
<storageType>numeric(10,6)</storageType>
|
|
797
|
<measurementScale>
|
|
798
|
<ratio>
|
|
799
|
<unit>
|
|
800
|
<standardUnit>dimensionless</standardUnit>
|
|
801
|
</unit>
|
|
802
|
<precision>0.000001</precision>
|
|
803
|
<numericDomain>
|
|
804
|
<numberType>real</numberType>
|
|
805
|
</numericDomain>
|
|
806
|
</ratio>
|
|
807
|
</measurementScale>
|
|
808
|
</attribute>
|
|
809
|
<attribute>
|
|
810
|
<attributeName>Longitude</attributeName>
|
|
811
|
<attributeDefinition>Longitude in geographic projection (decimal
|
|
812
|
degree)</attributeDefinition>
|
|
813
|
<storageType>numeric(10,6)</storageType>
|
|
814
|
<measurementScale>
|
|
815
|
<ratio>
|
|
816
|
<unit>
|
|
817
|
<standardUnit>dimensionless</standardUnit>
|
|
818
|
</unit>
|
|
819
|
<precision>0.000001</precision>
|
|
820
|
<numericDomain>
|
|
821
|
<numberType>real</numberType>
|
|
822
|
</numericDomain>
|
|
823
|
</ratio>
|
|
824
|
</measurementScale>
|
|
825
|
</attribute>
|
|
826
|
</attributeList>
|
|
827
|
</dataTable>
|
|
828
|
</dataset>
|
|
829
|
<additionalMetadata>
|
|
830
|
<metadata>
|
|
831
|
<stmml:unitList>
|
|
832
|
<stmml:unit name="pH units" unitType="undefined" id="pH units" parentSI="unknown"
|
|
833
|
multiplierToSI="1"> </stmml:unit>
|
|
834
|
<stmml:unit name="decimal degrees latitude" unitType="latitudeLongitude"
|
|
835
|
id="decimal degrees latitude" parentSI="unknown" multiplierToSI="1"> </stmml:unit>
|
|
836
|
</stmml:unitList>
|
|
837
|
</metadata>
|
|
838
|
</additionalMetadata>
|
|
839
|
</eml:eml>
|