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이재구,후르니에,Lee, Jae-Koo,Fournier, J.C. 한국응용생명화학회 1978 Applied Biological Chemistry (Appl Biol Chem) Vol.21 No.2
불란서(佛蘭西)의 수종(數種) 토양중(土壤中)에서 3,4-DCA 및 TCAB의 변화과정을 구명하기 위하여 환표식(環標識)된 $^{14}C-3,4-DCA$ 및 $^{14}C-TCAB$를 사용하여 실험을 행(行)한 바 다음의 결과(結果)를 얻었다. (1) $^{14}C-3,4-DCA$가 $^{14}CO_2$로 분해(分解)되는 속도(速度)는 배양초기(培養初期)에는 비교적(比較的) 빠르고 후기(後期)에는 완만하다. 배양 6개월 후(後)에 alkaline soil(pH=7.9)에서 dose 1(1.5 ppm)에서 최고(最高) 6.5%, dose 2(94 ppm)에서 최하(最下) 1.92%의 분해율(分解率)을 보였다. organic acid soil(pH=5.5)의 경우 dose 1에서 4.91%, dose 2에서 4.24%가 분해(分解)되었으며 양자간(兩者間)에는 대차(大差)가 없었다. (2) Dose 1로 3,4-DCA를 6개월동안 배양할 때 organic acid soil에서는 47.70%, Alkaline soil에서는 29.49%가 토양에 결합되었다. 한편 dose 2의 경우 organic acid soil에서는 38.40%, alkaline soil에서는 20.30%가 결합(結合)되었다. (3) 토양중(土壤中)에서 3,4-DCA로부터 생성(生成)되는 TC-AB의 양(量)은 토양(土壤)의 종류(種類)보다는 3,4-DCA의 사용농도(使用濃度)에 의존(依存)하는것 같다. dose 2에서 생성(生成)된 TCAB의 양(量)은 organic acid soil에서는 추출액(抽出液)의 총방사능(總放射能)의 50%, alkaline soil에서는 30%에 해당하며 이것은 토양시료(土壤試料)에 첨가한 최초(最初)의 방사능(放射能)의 1.8%와 1.4%에 각각(各各) 해당된다. 반면 dose 1에서는 추출액(抽出液)의 총방사능(總放射能)에 비(比)하여 두 토양(土壤) 공(共)히 $2{\sim}3%$를 넘지 못하며 최초(最初)의 총방사능(總放射能)의 $0.05{\sim}0.1%$를 초과(超過)하지 못한다. (4) $^{14}C-TCAB$가 $^{14}CO_2$로 분해(分解)되는 속도(速度)는 매우 느리며 배양 6개월후에 4종(四種)의 토양(土壤)에서 모두 $0.05%{\sim}0.20%$의 분해율(分解率)을 보였고 배양 3개월후에 뚜렷한 분해산물(分解産物)을 검출(檢出)할 수 없었으며 대부분(大部分) 미분해(未分解)된 상태로 존재(存在)하였다. (5) Alkaline soil에서 다른 토양에서 보다 훨씬 많은 양(量)의 $^{14}C-TCAB$가 토양중(土壤中)에 흡착(吸着)된 것으로 보아 Alkali토양 조건하에서 $trans-TCAB{\rightarrow}cis-TCAB$의 전환(轉換)이 일어나 이 흡착성이 더 강한 cis 이성체(異性體)가 토양중(土壤中)에 많이 흡착(吸着)된 것으로 생각(生覺)된다. In an attempt to elucidate the fate of 3,4-DCA and TCAB in various French soils, uniformly $^{14}C-ring-labeled$ 3,4-DCA and TCAB mere utilized and the following results obtained. 1) The rate of breakdown of $^{14}C-3,4-DCA$ into $^{14}CO_2$ was relatively higher in the early stage than that in the later stage. In 6 months of incubation in alkaline soil (pH 7.9), the rate was as high as 6.5% at dose 1 (1.5 ppm) and as low as 1.92% at dose 2(94 ppm), whereas in organic acid soil (pH 5.5) the rate was 4.91% at dose 1 and 4.24% at dose 2, respectively, without making any great difference between the two levels. 2) At dose 1, 47.70% of the initial radioactivity of $^{14}C-3,4-DCA$ was bound to soil in organic acid soil and 29.49% bound in alkaline soil, whereas at dose 2, 38.40% in organic acid soil and 20.30% in alkaline soil, respectively. 3) The amount of formation of $^{14}C-TCAB$ from $^{14}C-3,4-DCA$ seems to depend largely on the concentration of 3,4-DCA applied rather than on soil types. At dose 2, the amount was 50% of the total radioactivity extracted in organic acid soil and 30% in alkaline soil, corresponding to 1.8% and 1.4% of the initial radioactivity applied to soil, respectively. Cis-TCAB also seemed to be formed at dose 2 in both soils. Meanwhile, at dose 1, even though $^{14}C-TCAB$ was detected in trace on tlc and glc in both soils, the amount does not exceed 2 to 3% of the radioactivity extracted, corresponding to 0.05 to 0.1% of the initial radioactivity. 4) The rate of breakdown of $^{14}C-TCAB$ into $^{14}CO_2$ ranged from 0.05 to 0.20% in all the four soils. Most of the applied $^{14}C-TCAB$ remained intact after 3 months, not producing any detectable metabolites. 5) The fact that much more $^{14}C-TCAB$ was adsorbed to alkaline soil than to the other soils strongly indicates that in alkaline condition trans-isomer was converted tocisisomer which has the higher adsorption affinity than the former.
이재구,후르니에 한국농화학회 1978 Applied Biological Chemistry (Appl Biol Chem) Vol.21 No.2
In an attempt to elucidate the fate of 3, 4-DCA and TCAB in various French soils, uniformly ^(14)C-ring-labeled 3,4-DCA and TCAB mere utilized and the following results obtained. 1) The rate of breakdown of ^(14)C-3,4-DCA into ^(14)CO₂ was relatively higher in the early stage than that in the later stage. In 6 months of incubation in alkaline soil (pH 7.9), the rate was as high as 6.5% at dose 1 (1.5 ppm) and as low as 1.92% at dose 2(94 ppm), whereas in organic acid soil (pH 5. 5) the rate was 4.91% at dose 1 and 4.24% at dose 2, respectively, without making any great difference between the two levels. 2) At dose 1, 47.70% of the initial radioactivity of ^(14)C-3,4-DCA was bound to soil in organic acid soil and 29.49% bound in alkaline soil, whereas at dose 2, 38.40% in organic acid soil and 20.30% in alkaline soil, respectively. 3) The amount of formation of ^(14)C-TCAB from 14C-3, 4-DCA seems to depend largely on the concentration of 3, 4-DCA applied rather than on soil types. At dose 2, the amount was 50% of the total radioactivity extracted in organic acid soil and 30% in alkaline soil, corresponding to 1.8% and 1.4% of the initial radioactivity applied to soil, respectively. Cis-TCAB also seemed to be formed at dose 2 in both soils. Meanwhile, at dose 1, even though ^(14)C-TCAB was detected in trace on tlc and glc in both soils, the amount does not exceed 2 to 3% of the radioactivity extracted, corresponding to 0.05 to 0.1% of the initial radioactivity. 4) The rate of breakdown of ^(14)C-TCAB into ^(14)CO₂ ranged from 0.05 to 0.20% in all the four soils. Most of the applied ^(14)C-TCAB remained intact after 3 months, not producing any detectable metabolites. 5) The fact that much more ^(14)C-TCAB was adsorbed to alkaline soil than to the other soils strongly indicates that in alkaline condition trans-isomer was converted tocisisomer which has the higher adsorption affinity than the former.