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Zeman, L.J. (1975) Hydrochemical balance of a British Columbia mountainous watershed. CATENA, 2. 81-93 doi:10.1016/s0341-8162(75)80006-3

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Reference TypeJournal (article/letter/editorial)
TitleHydrochemical balance of a British Columbia mountainous watershed
JournalCATENA
AuthorsZeman, L.J.Author
Year1975 (January)Volume2
PublisherElsevier BV
DOIdoi:10.1016/s0341-8162(75)80006-3Search in ResearchGate
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Mindat Ref. ID16574811Long-form Identifiermindat:1:5:16574811:7
GUID0
Full ReferenceZeman, L.J. (1975) Hydrochemical balance of a British Columbia mountainous watershed. CATENA, 2. 81-93 doi:10.1016/s0341-8162(75)80006-3
Plain TextZeman, L.J. (1975) Hydrochemical balance of a British Columbia mountainous watershed. CATENA, 2. 81-93 doi:10.1016/s0341-8162(75)80006-3
In(1975) CATENA Vol. 2. Elsevier BV

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Millward, Andrew A, Mersey, Janet E (1999) Adapting the RUSLE to model soil erosion potential in a mountainous tropical watershed. CATENA, 38 (2) 109-129 doi:10.1016/s0341-8162(99)00067-3
Meyer, B. (1975) CATENA, 2. Elsevier BV. 201-202 doi:10.1016/s0341-8162(75)80013-0
(2010) Editorial Board. CATENA, 81 (3) doi:10.1016/s0341-8162(10)00065-2
Avery, B.W. (1993) Defining kinds of soil horizon. CATENA, 20 (4) 403 doi:10.1016/s0341-8162(05)80006-2
Knoblich, Klaus (1975) Über Den Böschungswinkel Von Schutthalden. CATENA, 2. 1-10 doi:10.1016/s0341-8162(75)80001-4
Zakaria, A.S. (1975) The geomorphology of Kelantan Delta (Malaysia) CATENA, 2. 337-349 doi:10.1016/s0341-8162(75)80021-x
Höllermann, Peter (1975) Formen Kavernöser Verwitterung (“Tafoni”) Auf Teneriffa. CATENA, 2. 385-409 doi:10.1016/s0341-8162(75)80024-5
Ruhe, Robert V. (1975) Climatic geomorphology and fully developed slopes. CATENA, 2. 309-320 doi:10.1016/s0341-8162(75)80019-1
(2008) Editorial Board. CATENA, 75 (2) doi:10.1016/s0341-8162(08)00137-9
(2010) Editorial Board. CATENA, 81 (2) doi:10.1016/s0341-8162(10)00035-4
Culling, W.E.H. (1986) Highly erratic spatial variability of soil-pH on Iping Common, West Sussex. CATENA, 13 (1) 81-98 doi:10.1016/s0341-8162(86)80006-6
 
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