• Bulletin of the Korean Chemical Society
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• 제9권6호
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• pp.365-368
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• 1988

Coordination chemistry of organotin(IV) dithiocarbamate complexes has been examined in terms of far infrared and $^{119}Sn$-NMR spectroscopies. Although the Sn-S stretching vibrational bands of the complex could not be correlated with the bonding nature of the dithiocarbamate ligand, $^{119}Sn$ chemical shifts were sensitive enough to distinguish clearly the coordination number of tin, and as such the bonding mode of the dithiocarbamate ligand could be indentified to be monodentate or bidentate. Thus the $^{119}Sn$-NMR study on new cyclohexyltin(IV) dithiocarbamate complexes along with the known complexes suggests that the bonding mode of the dithiocarbamate ligands and the consequent coordination number of tin are determined mainly by the inductive effects of the organic groups attached to the tin atom.

• Bulletin of the Korean Chemical Society
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• 제26권6호
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• pp.892-898
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• 2005

A long, bis(monodentate), linking Schiff-base ligand L (py-CH=N-$C_6H_4$-N=CH-py) was prepared from 1,4-phenylenediamine and 3-pyridinecarboxaldehyde by the Schiff-base condensation. Ligand L has two terminal pyridyl groups capable of coordinating to metals through their nitrogen atoms. In contrast, the same reaction between 1,2-phenylenediamine and 3-pyridinecarboxaldehyde produced a mixture of imidazol isomers (2-pyridin-3-yl-1H-benzoimidazole), which are connected to one another by the N-H…N hydrogen bonding to form a tetramer. From Zn($NO_3)_2{\cdot}6H_2O$ and ligand L under various conditions, one discrete molecule, trans- [Zn($H_2O)_4L_2]{\cdot}(NO_3)_2{\cdot}(MeOH)_2$, and two 1-D zinc polymers, [Zn$(NO_3)(H_2O)_2(L)]{\cdot}(NO_3){\cdot}(H_2O)_2$ and [Zn(L) (OBC)($H_2O$)], were prepared. In ligand L, the N$\ldots$N separation between the terminal pyridyl groups is 13.994 $\AA$, with their nitrogen atoms at the meta positions (3,3’) in a trans manner. The corresponding N$\ldots$N separations in its compounds range from 13.853 to 14.754 $\AA$.

• 한국토양비료학회지
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• 제29권2호
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• pp.107-112
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• 1996

토양의 규산 흡착기작을 밝히고자 continuous stirred-flow(연속진탕흘림) 법을 이용하여 시간 경과에 따른 규산 흡착량 변화에 대한 실험을 $25^{\circ}C$, pH 3수준(5, 6.5, 8)에서 실시하였다. 규산 흡착량은 실험기간내 최대 흡착량을 보이지 않고 계속 증가 하였다. 시간에 따른 규산의 흡착과정을 2단계로 구분 하였고, 1단계 반응과정은 아래의 지수함수식에서 고도의 유의성있는 상관관계를 보였다 $$R_{ad}=K_a*(Q_{OH}^S)^n$$ 여기서 $R_{ad}$는 규산흡착속도($Si\;{\mu}mal/min$), $Q_{OH}^S$는 알칼리 투여를 통하여 생성된 토양표면 음전하량, $K_a$와 n 은 상수이다. 1단계 반응과정의 n값은 1.1로 한자리 결합(monolantate ligand bonding)에 의한 흡착과정인 것으로 나타났다. 2단계 과정은 아래 식에서 고도의 유의성있는 상관관계를 보였다. $$R_{ad}=K_b*(pH)$$ 이때 $K_b$ 는 비례상수로, pH 증가에 따른 규산 흡착 속도의 증가 추세가 지수 함수적으로 감소하는 경향을 보였다.