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Çѱ¹ÀܵðÇÐȸ / v.9, no.4, 1995³â, pp.275-284
°ü¾Ç»êÀÇ Àܵð¿Í ¾ï»õ »ýŰ迡 À־ ¿¡³ÊÁöÀÇ È帧°ú ¹«±â¹°ÀÇ ¼øÈ¯ 4.ÀÎÀÇ ¼øÈ¯
( The Energy Flow and Mineral Cycles In a Zoysia japonica and a Miscanthus sinensis Ecosystem on Mt. Kwanak 4. The Cycles of Phosphorus )
Àå³²±â;±èÁ¤¼®;°­°æ¹Ì; ¼­¿ï´ëÇб³ »ý¹°±³À°°ú;¼­¿ï´ëÇб³ »ý¹°±³À°°ú;¼­¿ï´ëÇб³ »ý¹°±³À°°ú;
 
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In this investigation, the accumulation mineralization and annual cycle of organic P has been studied in grassland ecosysterns of a Z japonica grassland and a M sinensis grassland on Mt. Kwanak. The basic models of the accumulation and mineralization for ash components of a grass-litter have been presented as the equations (1), (2), and (3). The equations (7)~(10) for organic P are derived from these basic concepts. There was a highty significant relationship between organic matter and organic P. The estimates between organic matter and organic P correlated very high significance. The parameter factors k or k' of mineralization of organic P for the Z. japonica and M sinensis asslands were k=0.412 or k'=0.292 and k=0.224 or k'=0.183, respectively. The time required for a cycle to be completed from organic P to inorganic P of 50, 95 and 99 % are 3.9, 16.7 and 27.8 years in the Z. japonica grassland and 4.1, 17.7 and 29.4 years in the M sinensis grassland. The annual P cycle formulae for mineralization were based on the equations (5), (11) and (12). Annual yields of mineralization for organic P in the steady state grasslands of Z. japonica and M sinensis were 0.407 and 0.504g /$m^2$, respectively. Key words : Zoysia japonica Miscanthus sinensis Mt. Kwariak, Phosphorus cycles
 
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Zoysia japonica;Miscanthus sinensis;Mt;Kwanak;Phosphorus cycles;
 
Çѱ¹ÀܵðÇÐȸÁö / v.9, no.4, 1995³â, pp.275-284
Çѱ¹ÀܵðÇÐȸ
ISSN : 1229-3253
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO199511920301998)
¾ð¾î : Çѱ¹¾î
³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø
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