共查询到8条相似文献,搜索用时 72 毫秒
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为了研究稀土离子与氨基酸 (Pro)的相互作用 ,在pH≈ 3.5水溶液中合成了高氯酸八水·(脯氨酸 )合铱 (Ⅲ )铒 (Ⅲ ) ,获得了单晶 ,并经四圆衍射仪测定了结构 .配合物组成为C2 0 H52 Cl6ErN4 O4 0 Y ,属三斜晶系 ,P1空间群 .晶胞参数a =0 .986 0 (2 )°nm ,b =1.30 2 0 (5 )nm ,c=1.36 32 (5 )nm ,α =10 9.32 (3)° ,β=110 .19(2 )° ,γ =10 0 .96 (2 )°,V =1.45 6 (1)nm3,Z =1,Dc=1.6 6 3g/cm3,μ =2 .797mm-1,F(0 0 0 ) =72 9.配合物分子中 ,Y3 ‘、Er3 在相应位置上出现的几率各为 5 0 % ,相邻两个金属离子被两个以桥式双齿配位的Pro分子连接 ,每个金属离子除了与 4个羧基O配位外 ,还与 4个水分子的氧配位 ,配位数为 8,形成变形的四方反棱柱 .图 4表 3参 10 相似文献
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单甲脒水中溶解度及正辛醇/水分配系数的测定 总被引:4,自引:5,他引:4
有毒有机化合物在水中的溶解度(WS)及正辛醇/水分配系数(K_(ow)),是描述其在环境中行为的两个重要物理化学参数。本文用溶解度平衡曲线法和振荡法,测得单甲脒在水中的溶解度为21.8±1.3mg/1(25℃),其在正辛醇/水中的分配系数lgK_(ow)为2.92±0.06。 相似文献
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单甲脒在土壤中的降解及持久性研究 总被引:3,自引:0,他引:3
本文对四种不同类型土壤中单甲脒及其盐酸盐在厌氧与好氧条件下的降解动态及其残留进行了研究。结果表明单甲脒及其盐酸盐均属不稳定的化合物,单甲脒在土壤中的半衰期为4.6-9.1d,其盐酸盐的半衰期为2.0-6.2d。结果还表明单甲脒盐酸盐在厌氧条件下较在好氧条件下降解缓慢;在厌氧条件时,土壤的pH值对其降解影响较大。在相同条件下,单甲脒比它的盐酸盐酸盐降解慢,其降解速率与土壤pH值无关。 相似文献
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The distribution of three important dissolved forms of nitrogen, viz. nitrate, nitrite and urea in the surface and bottom water samples collected from 27 selected hydrographic profiles, in the Arabian Sea, along the west coast of India is described. Of the three forms, nitrate concentrations were the highest and comparatively higher concentrations were observed in the bottom water. Decomposition of organic matter resulting in the release of the thermodynamically stable nitrogen species, i.e. nitrate, may be the major factor resulting in higher nitrate concentrations at these depths, where the water is also characterized by low values of dissolved oxygen and temperature. The significant positive correlation between A.O.U. and nitrate of the bottom water samples emphasizes the role of oxidative decomposition of organic matter which plays an active role in reducing the oxygen concentrations below the theoretical values since at this depth ( ≈200 m) the net production is taken to be zero. This is also evidenced by the negative correlation of nitrate with dissolved oxygen and temperature, for the bottom samples. 相似文献