32,394 research outputs found

    Mueller, R H, VX29510

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    This record was harvested from a previous catalogue system and will be withdrawn in 2025. Information in this record may be superseded or incomplete. Visit this record in UMA's new catalogue at: https://archives.library.unimelb.edu.au/nodes/view/406548Surname: MUELLER. Given Name(s) or Initials: R H. Military Service Number or Last Known Location: VX29510. Missing, Wounded and Prisoner of War Enquiry Card Index Number: 31665.247908 Item: [2016.0049.38825] "Mueller, R H, VX29510

    Letters between Dr. George Fordyce Story, Tasmania and Baron Ferdinand von Mueller, Melbourne 1867-1871

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    Correspondence between Ferdinand von Mueller, Director of the Melbourne Botanical Gardens and Dr. George Fordyce Story, Tasmania. Story supplied Mueller with plants and in return Mueller gave him information about them. From Cotton Family Papers C7/72 - 85......Please note, the first letter: "Letter von Mueller to Story, 1867" has been previously transcribed and published in: "Regardfully Yours: Selected Correspondence of Ferdinand von Mueller, vol II: 1860 - 1875" edited by R. W Home, A.M Lucas, Sara Maroske, D.M Sinkora and J. H Vogit, p. 412 (UTAS Library reference: Science QK 31. M75 A4 1998 vol. 2). Letters transcribed by Sarah Clarkson, University of Tasmania

    Mueller, Mrs. H. [with Child]; Portraits - 1914

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    Photograph of a woman and child; the woman is identified as Mrs. H. Mueller. She is holding the infant, and they are both wrapped in a light-colored cloth

    Importance of vegetation, topography and flow paths for water transit times of base flow in alpine headwater catchments

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    The mean transit time (MTT) of water in a catchment gives information about storage, flow paths, sources of water and thus also about retention and release of solutes in a catchment. To our knowledge there are only a few catchment studies on the influence of vegetation cover changes on base flow MTTs. The main changes in vegetation cover in the Swiss Alps are massive shrub encroachment and forest expansion into formerly open habitats. Four small and relatively steep headwater catchments in the Swiss Alps (Ursern Valley) were investigated to relate different vegetation cover to water transit times. Time series of water stable isotopes were used to calculate MTTs. The high temporal variation of the stable isotope signals in precipitation was strongly dampened in stream base flow samples. MTTs of the four catchments were 70 to 102 weeks. The strong dampening of the stable isotope input signal as well as stream water geochemistry points to deeper flow paths and mixing of waters of different ages at the catchments' outlets. MTTs were neither related to topographic indices nor vegetation cover. The major part of the quickly infiltrating precipitation likely percolates through fractured and partially karstified deeper rock zones, which increases the control of bedrock flow paths on MTT. Snow accumulation and the timing of its melt play an important role for stable isotope dynamics during spring and early summer. We conclude that, in mountainous headwater catchments with relatively shallow soil layers, the hydrogeological and geochemical patterns (i.e. geochemistry, porosity and hydraulic conductivity of rocks) and snow dynamics influence storage, mixing and release of water in a stronger way than vegetation cover or topography do

    Franz H. Mueller, The Church and the Social Question, 1984

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    Daude Jeannine. Franz H. Mueller, The Church and the Social Question, 1984. In: Revue Française d'Etudes Américaines, N°26, novembre 1985. Le paysage américain. p. 473

    041. 11-15-78 Luke 21:18

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    Chapel Sermon by H Mueller on Wednesday, November 15, 1978

    Author response; Peter Mueller

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