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Possible water flow into Mud Lake Bog.
dc.contributor.authorDewoina, Kathleenen_US
dc.coverage.spatialInverness Mud Lake Bogen_US
dc.date.accessioned2007-06-14T18:10:52Z
dc.date.available2007-06-14T18:10:52Z
dc.date.issued1974en_US
dc.identifier.urihttps://hdl.handle.net/2027.42/52798
dc.description.abstractEvidence for considerable ground water flow into Mud Lake bog, Cheboygan County, Michigan. Ground water seems to be the source of minerals maintaining high conductivity and alkalinity in Mud lake bog. The bog has a large sphagnum mat area which could be responsible for a high rate of efflux of dissolved minerals from the bog water proper.en_US
dc.format.extent2601498 bytes
dc.format.extent3144 bytes
dc.format.mimetypeapplication/pdf
dc.format.mimetypetext/plain
dc.relation.haspartGraphen_US
dc.relation.haspartMapen_US
dc.relation.haspartTable of Numbersen_US
dc.subjectWinter Ecologyen_US
dc.subject.classificationBogen_US
dc.subject.otherGROUNDWATERen_US
dc.subject.otherWATERen_US
dc.subject.otherCHEMISTRYen_US
dc.subject.otherMINERALSODIUMen_US
dc.subject.otherPOTASSIUMen_US
dc.subject.otherMAGNESIUMen_US
dc.subject.otherPHOSPHATEen_US
dc.subject.otherNITRATEen_US
dc.subject.otherCALCIUMen_US
dc.subject.otherPHen_US
dc.subject.otherCONDUCTIVITYen_US
dc.subject.otherALKALINITYen_US
dc.titlePossible water flow into Mud Lake Bog.en_US
dc.typeWorking Paperen_US
dc.subject.hlbsecondlevelNatural Resource and Environmenten_US
dc.subject.hlbtoplevelScienceen_US
dc.contributor.affiliationumBiological Station, University of Michiganen_US
dc.contributor.affiliationumcampusAnn Arboren_US
dc.description.bitstreamurlhttp://deepblue.lib.umich.edu/bitstream/2027.42/52798/1/1231.pdfen_US
dc.description.filedescriptionDescription of 1231.pdf : Access restricted to on-site users at the U-M Biological Station.en_US
dc.owningcollnameBiological Station, University of Michigan (UMBS)


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