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  • Extracting cores from a tree using an increment borer has been standard practice in den-drochronological studies for a long time. Although empirical rules exist regarding how many samples to take and which methodology to apply, comparatively few studies provide quantification of the sim-ilarity of relative tree-ring-widths (TRW) around the stem circumference. The aim of this study was therefore to precisely measure the similarity of standardised TRWs around the stem circumference and to provide objective suggestions for optimal core sampling of Norway spruce (Picea abies Karst. [L.]) and European beech (Fagus sylvatica L.) growing in Central European temperate forests. A large sample of cross-sectional discs was used from Norway spruce and European beech trees growing on various slopes, at different altitudes and biogeographic regions across the Czech Republic and Slovakia. The similarity of TRWs measured in different coring directions was analysed by testing the relativized TRW arou
  • Extracting cores from a tree using an increment borer has been standard practice in den-drochronological studies for a long time. Although empirical rules exist regarding how many samples to take and which methodology to apply, comparatively few studies provide quantification of the sim-ilarity of relative tree-ring-widths (TRW) around the stem circumference. The aim of this study was therefore to precisely measure the similarity of standardised TRWs around the stem circumference and to provide objective suggestions for optimal core sampling of Norway spruce (Picea abies Karst. [L.]) and European beech (Fagus sylvatica L.) growing in Central European temperate forests. A large sample of cross-sectional discs was used from Norway spruce and European beech trees growing on various slopes, at different altitudes and biogeographic regions across the Czech Republic and Slovakia. The similarity of TRWs measured in different coring directions was analysed by testing the relativized TRW arou (en)
Title
  • EVALUATING SIMILARITY OF RADIAL INCREMENTS AROUND TREE STEM CIRCUMFERENCE OF EUROPEAN BEECH AND NORWAY SPRUCE FROM CENTRAL EUROPE
  • EVALUATING SIMILARITY OF RADIAL INCREMENTS AROUND TREE STEM CIRCUMFERENCE OF EUROPEAN BEECH AND NORWAY SPRUCE FROM CENTRAL EUROPE (en)
skos:prefLabel
  • EVALUATING SIMILARITY OF RADIAL INCREMENTS AROUND TREE STEM CIRCUMFERENCE OF EUROPEAN BEECH AND NORWAY SPRUCE FROM CENTRAL EUROPE
  • EVALUATING SIMILARITY OF RADIAL INCREMENTS AROUND TREE STEM CIRCUMFERENCE OF EUROPEAN BEECH AND NORWAY SPRUCE FROM CENTRAL EUROPE (en)
skos:notation
  • RIV/60460709:41320/14:65223!RIV15-MZE-41320___
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • P(QI102A079)
http://linked.open...iv/cisloPeriodika
  • 2
http://linked.open...vai/riv/dodaniDat
http://linked.open...aciTvurceVysledku
http://linked.open.../riv/druhVysledku
http://linked.open...iv/duvernostUdaju
http://linked.open...titaPredkladatele
http://linked.open...dnocenehoVysledku
  • 15288
http://linked.open...ai/riv/idVysledku
  • RIV/60460709:41320/14:65223
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • relative tree-ring width, dendroclimatology, basal area reconstruction, core sampling, detrending (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • CZ - Česká republika
http://linked.open...ontrolniKodProRIV
  • [358192378624]
http://linked.open...i/riv/nazevZdroje
  • Geochronometria
http://linked.open...in/vavai/riv/obor
http://linked.open...ichTvurcuVysledku
http://linked.open...cetTvurcuVysledku
http://linked.open...vavai/riv/projekt
http://linked.open...UplatneniVysledku
http://linked.open...v/svazekPeriodika
  • 41
http://linked.open...iv/tvurceVysledku
  • Sedmák, Róbert
  • Bošeľa, Michal
  • Marušák, Róbert
  • Petráš, Rudolf
  • Barna, Milan
  • Sedmáková, Denisa
http://linked.open...ain/vavai/riv/wos
  • 000338330300004
issn
  • 1733-8387
number of pages
http://bibframe.org/vocab/doi
  • 10.2478/s13386-013-0152-3
http://localhost/t...ganizacniJednotka
  • 41320
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