CAJ | 학술논문

根据近年作者及相关研究成果，提出一般茶园（非F污染区，非高F地质背景区）生态系统F的生物地球化学循环模型，估算茶园生态系统各子系统F的库容和库之间的F流量，分析茶园生态系统F的生物地球化学特征．结果表明：1）茶园生态系统F的惰性库：调节库：活动库为239：4：1，活动库占总库容的比例高达0．41％，其比例是非常高的；2）该生态系统F的外循环是一个正平衡循环，F的收入与支出比为2：1，同时地表径流的F支出大于地下径流的F支出；3）由于茶树具有很强的从土壤摄取F的能力，摄取的F绝大部分（98％）汇集于叶上，特别是老叶上，且部分易被雨水淋出，因而通过透冠流和枯枝落叶形成很大的F流量，分别达10．5k·hm^-2·a^-1和8．5kg·hm^-2·a^-1，内循环流量达19．95kg·hm^-2·a^-1，为活动库库容的3．6倍，使活动库具有很高的更新速率；4）茶园生态系统F的生物地球化学循环伴随着系统中F的活化、有机化和生物积累过程．
근거근년작자급상관연구성과，제출일반다완（비F오염구，비고F지질배경구）생태계통F적생물지구화학순배모형，고산다완생태계통각자계통F적고용화고지간적F류량，분석다완생태계통F적생물지구화학특정．결과표명：1）다완생태계통F적타성고：조절고：활동고위239：4：1，활동고점총고용적비례고체0．41％，기비례시비상고적；2）해생태계통F적외순배시일개정평형순배，F적수입여지출비위2：1，동시지표경류적F지출대우지하경류적F지출；3）유우다수구유흔강적종토양섭취F적능력，섭취적F절대부분（98％）회집우협상，특별시로협상，차부분역피우수림출，인이통과투관류화고지락협형성흔대적F류량，분별체10．5k·hm^-2·a^-1화8．5kg·hm^-2·a^-1，내순배류량체19．95kg·hm^-2·a^-1，위활동고고용적3．6배，사활동고구유흔고적경신속솔；4）다완생태계통F적생물지구화학순배반수착계통중F적활화、유궤화화생물적루과정．
Based on the data from recent researches, a model on the biogeochemical cycle of F in tea garden ecosystem was conceptualized, and the capacity of F pools, the flows of F between the components and characteristics of the ecosystem were analyzed. Results indicated： 1 ） The capacity proportions of the inert pool, regulate pool and active pool of F in the ecosystem are 239 ：4 ： 1. The active pool occupies a great proportion of 0. 41% in total F of the system; 2） The outside cycle of F shows a positive balance, the proportion of receipts to expenditures of F amounts to 2 ： 1, and the expenditure of F is more through surface water than through groundwater; 3 ） There is a strong inner cycle of F （19.95 kg. hm-2 .a-1） in the tea garden ecosystem, because F is absorbed largely from soil by tea plant （18.62 kg .hm-2 . a-1） and stored mainly in the leaves （98%）, especially in old leaves, but largely returns to soil by leaching rainwater （ 10. 49 kg . hm-2 . a-1 ） , and by dead branches and leaves （8.54 kg . hm -2 . a-1 ） , the amount of F in inner cycle capacity of active pool, leading equals to a fast replacement rate of F in the chemical cycle of F is accompanied by processes such as F activation, compound form and F biological accumulation in tea garden ecosystem. 3.6 times as much as the F- active pool; 4） The biogeo- F transformation into organic