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Fastlink of full TGIF record #69383

The fastlink for this record is: https://tic.msu.edu/tgif/flink?recno=69383
Full TGIF Record # 69383
Item 1 of 1
Publication Type:
i
Report
Author(s):Kamon, Yasuhiko
Author Affiliation:KGU Green Research Center
Title:Dojyou sosei ga dojyou buturisei oyobi kouraishiba ikusei ni ataeru eikyou
Translated Title:Effects of soil texture for soil physical laws and Zoysiagrass growing
Article Series:Effects of soil texture, Part 1
Section:Research article
Other records with the "Research article" Section
Source:Turf Research Bulletin [Kansai Golf Union Green SectionResearch Center] [Gurin Kenkyo Hokokushu]. Vol. 36, March 1979, p. 59-72.
# of Pages:14
Publishing Information:Takarazuka, Japan: Kansai Golf Union Green Section Research Center [Kansi Goruhu Renmei Gurin Kenkyujo]
Keywords:TIC Keywords: Soil texture; Physical properties of soil; Zoysia; Sod; Sodding; Transplanting; Roots; Shoot growth; Comparisons; Root growth; Growth rate
Abstract/Contents:"Soil is [a] very important factor to hopeful grow [growth] of turfgrasses, and improvement of soil physical lows after sodding are impossible [to] expect to refresh build soil bed. This [These] lows are almost decided by soil texture for soil physical laws and zoysiagrass growing, and soil of each plot is shown in table-1. Generally root response of zoysiagrass sods after transplanting is said [to be a] better soil than sand. However this is caused by soil moisture difference after transplanting, rooting is not difference in enough irrigation. (table-2) The total fresh weight of shoot growth are more E and G than A and B, and shoot growths of each cutting day are [the] same result for 1~2 monthes [months] after transplanting (Figure-9,-10,-11). This result prove [proves] that the good quarity [quality] of zoysiagrass are built more fast [faster] [in] soil bed than sand bed. However root growing is more A and B than E and G. (Figure-15). Shoot and root growth are inverse, but this will be due to rate of soil solids, soil water and soil air. These are much different of A, B and G,E. The rate of soil solids, soil water and soil air are different in each soil and depth(Figure-16. Table-5,-6). The good rate of these three phase [phases] are C and D, but these rate [rates] are shown by non tread conditions, so these rate [rates] will be changed by tread condition."
Language:Japanese
References:8
See Also:See also part 2, "Dojousosei ga dojou butsurisei oyobi Koraishiba ikuseini ataeru eikyou [Effects of soil texture for soil physical laws and Zoysiagrass growing]", Vol. 37, July 1979, p. 55-66, R=79362 R=79362

See also part 3, "Dojousosiki ga dojoubutsurisei oyobi Koraishiba ikusei ni ataeru eikyou [Effects of soil texture for soil physical laws and Zoysiagrass growing]", Vol. 39, August 1980, p. 63-72, R=79468 R=79468
Note:English summary appears
Pictures, b/w
Figures
Tables
Graphs
ASA/CSSA/SSSA Citation (Crop Science-Like - may be incomplete):
Kamon, Y. 1979. Dojyou sosei ga dojyou buturisei oyobi kouraishiba ikusei ni ataeru eikyou. (In Japanese) Turf Res. Bull. 36:p. 59-72.
Fastlink to access this record outside TGIF: https://tic.msu.edu/tgif/flink?recno=69383
If there are problems with this record, send us feedback about record 69383.
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MSU catalog number: SB 433 .G87
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