THE JOURNAL OF THE JAPANESE FORESTRY SOCIETY
Online ISSN : 2185-8195
Print ISSN : 0021-485X
ISSN-L : 0021-485X
Volume 34, Issue 2
Displaying 1-9 of 9 articles from this issue
  • Ken-ichi HATANO
    1952Volume 34Issue 2 Pages 37-41
    Published: February 25, 1952
    Released on J-STAGE: September 02, 2011
    JOURNAL FREE ACCESS
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  • Hiroyuki ITO
    1952Volume 34Issue 2 Pages 42-43
    Published: February 25, 1952
    Released on J-STAGE: September 02, 2011
    JOURNAL FREE ACCESS
    (1) One flavanone derivative, m. p. 265-266°C is obtained from the wood of Prunus serrata var. spontanea S. et Z. through the procedure of the lead-salt precipitation.
    (2) This product is identified with known Eriodictyol (4′, 5, 5′, 7-tetrahydroxyflavanone) from the standpoint of its physical characteriatics and chemical properties.
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  • On the felling and transportation of Shii and Tabu
    Shoichi MIYOSHI, Yoshimi OGATA
    1952Volume 34Issue 2 Pages 43-45
    Published: February 25, 1952
    Released on J-STAGE: September 02, 2011
    JOURNAL FREE ACCESS
    Shii and Tabu at the natural broad-leabed forests in Miyazaki have been used for the f firewood. Recent experiments show that they can be used as pulp-wood, and we studied the processes of felling, pruning, bucking barking and transportation for the pulp-wood and for the charcoal-wood respectively. Then the unit stumpage value was calculated. The result is that the price for the pulp-wood is 214% higher than that of the charcoal-wood. Such utilization of Shii and Tabu is more profitable and will be of much use for the improvement of that natural forests.
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  • Rikizo NISHI, Daizo KIMURA
    1952Volume 34Issue 2 Pages 45-47
    Published: February 25, 1952
    Released on J-STAGE: September 02, 2011
    JOURNAL FREE ACCESS
    It is an important work method in the erosion control to prepare the channel, but none of the formulas of velocity of water current which has been known up to date are available for the plan of the steep open channel.
    We, therefore, measured the velocities of water in many open channel made of concrete at various places of southern Kyushyu.
    If we apply the Bernoulli's theorem between the upper and lower points of the channel, then we have V22=V21+2gh-2gh′.
    The value of h′ (friction head) calculated from the value of measurements is written h′ =K(V1+V2)2/4Rh, where R is hydraulic mean depth, then we have the value of coefficient K.
    If we put K2g/4RK, then the velocity V2 when the water current flowing in the velocity V1 in a given point passed through the vertical height h of the steep open channel can be obtained by the formula V2=√V21+2gh(1+K′h)-K′hV1/1+K′h
    The value of K′ obtained form the present measurement is not sufficient to draw the conclusion as shown in the preceeding table, and we intend to study it more critically in the near future.
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  • Thermal decomposition of the wood of Quercus glauca and its methanol-lignin
    Takeo SHIBAMOTO, Kyoji MTNAMI, Kenjiro ENDO
    1952Volume 34Issue 2 Pages 48-52
    Published: February 25, 1952
    Released on J-STAGE: September 02, 2011
    JOURNAL FREE ACCESS
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  • Reaction of HClO4 to cellulose and wood
    Hisao ISHIKAWA, Toshihiro KÔNO
    1952Volume 34Issue 2 Pages 52-56
    Published: February 25, 1952
    Released on J-STAGE: September 02, 2011
    JOURNAL FREE ACCESS
    By a reaction of HClO4 to native cellulose, hydroxyethyl cellulose and wood, we show as follows;
    1). Mechanism for a reaction of HClO4 to cellulose included in wood was much the same with it to native cellulose (cotton and pulp celluloses) and the limit concentration of HClO4 between the intermicelliar and intramicelliar reaction to cellulose was about 50%.
    2). Percentage of the lignin residues that were isolated from the 75% HClO4 treated wood powders by washing with the same concentration of HClO4, was 96.15% of 66% H2SO4 lignin.
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  • Goro TAKASE
    1952Volume 34Issue 2 Pages 56-60
    Published: February 25, 1952
    Released on J-STAGE: September 02, 2011
    JOURNAL FREE ACCESS
    A. On the asumption that the volume of cut logs can be shown practically by the following formula, experimental formulas were led from the research data of 292, logs of SUGI, all being 4 meters long but various diameters.
    V=(a+bG0+cG1dγ+eG2+fGn)
    The reason of assuming the above formula are as follows:
    1, Most of the cubing formulas of cut logs used in the past are the abbriviated forms of the above.
    2, As suggestible by the disgrams of V, G0, G1, γ, G2, Gn, volume (V) can be shown by the formula:
    V=a+bGi(Gi: G0, G1, γ, G2, Gn)
    B. Among the following experimental formlas including one section out of five, there is no significant difference for 1% leyel of significance.
    V=+0.004604+3.845182G1 S=0.035044
    V=+0.000616+4.153769γ S=0.031051
    V=+0.003569+4.409815G2 S=0.035937
    C, Among the following experimental formulas including 2 sections out of 5, there is no significant difference fox 1% level of significance.
    V=+0.000465+0.438407G0+3.489420γ
    S=0.01867
    V=+0.003939+0.501401G0+3.606105G2
    S=0.01883
    V=-0.001393+1.959273G1+2.185832G2
    S=0.01939
    V=+0.003024+1.762613G1+2.265029γ
    S=0.02147
    D. Among the following experimental form ulas including 3 sections out of five, there is no significant difference for 1% level of significance.
    V=+0.001744+0.4281G0+1.7929γ+1.8298G2
    S=0.0125
    V=+0.000490+0.3468G0+1.3167G1+2.3593G2
    S=0.0130
    V=+0.002420+0.4089G0+2.5212γ+1.1499Gn
    S=0.0148
    E. The experimental formula including all 5 sections is:
    V=+0.000909+0.3487G0+0.8054G1+1.1935γ+1.3360G2+0.3619Gn S=0.010619
    F. When the volumes accounted by Huber's formula Smalian's formula, Simony's formula. Shiffel's formula, and Wada's formula are compared with the volume by the experimental formulas including the same section or sections that the above various formulas have, there are significant difference for 1% or 5% level of significance, as follows:
    Huber's f. V=γ×l S=0.0432
    Exp. f. V=(+0.00015+1.038442γ)×l S=0.0311
    Smalian's f. V=(0.5G0+0.5Gn)×l S=0.3356
    Exp. f. V=(+0.002293+0.138398G0+0.926559Gn)×l S=0.0373
    Simony's f. V=(0.6667G1+0.3333γ+0.6667G2)×l S=0.0310
    Exp. f.V=(-0.004051+0.3784G1+0.2840γ+0.3729G2)×l S=0.0176
    Riecke's f. V=(0.1667G0+0.6667γ+0.1667Gn)×l S=0.0227
    Wada's f. V=(0.074G0+0.798γ+0.136Gn×l S=0.0214
    Exp. f. V=(+0.00605+0.1022G0+0.6303γ+0.2875Gn)×l S=0.0148
    Siffel's f. V=(0.61G1-0.23√G1G2-0.62G2)×l S=0.0294
    Exp. f. V=(-0.000435+0.2878G1+0.5019 √G1G2+0.2412G2)×l S=0.0162
    G. For the above reason, it seems to be necessity to amend the coefficient of the cubing formulas used in the past to aply to the logs of SUGI, 4 meters long.
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  • [in Japanese]
    1952Volume 34Issue 2 Pages 61-62
    Published: February 25, 1952
    Released on J-STAGE: September 02, 2011
    JOURNAL FREE ACCESS
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  • [in Japanese]
    1952Volume 34Issue 2 Pages 62-63
    Published: February 25, 1952
    Released on J-STAGE: September 02, 2011
    JOURNAL FREE ACCESS
    Download PDF (351K)
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