63 resultados para UCPR r 229(1)(b)


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穿透雨量是林内有效雨量的主要组成部分 ,其量能占 90 %以上。由于林冠空间分布的不均匀性 ,难以对林内穿透雨量进行精确地测量。从林冠截留降雨的作用机理出发 ,在做出几个假设的基础上 ,用数学方法建立了林内穿透雨量模型 ,即 :当 PR=P- α W[1 - ( 1 - P/U) b+ 1]   ( b>0 ,U>0 )当 P≥ U时 ,R=P- W其中 U=W( b+ 1 ) ,式中 b,W,U为模型参数 ,R为林内穿透雨量 ,P为大气降雨量 ,α为林分郁闭度。结合两个有实测资料的针叶树林分 ,又进一步介绍了模型参数的确定方法。同时将模型的计算结果与实测数据进行了对比 ,两者吻合性很好 ,验证效果是比较理想的。模型概念清晰 ,参数物理意义明确。在风速和雨强不太大的情况下 ,本模型适用于任何林分的穿透雨量的计算。然而 ,为了应用于无实测资料地区 ,尚须进一步研究模型参数与林分特征的关系。

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The first aryldiimine NCN-pincer ligated rare earth metal dichlorides (2,6-(2,6-C6H3R2N=CH)(2)C6H3)LnCl(2)(THF)(2) (Ln = Y, R = Me (1), Et (2), Pr (3); R = Et, Ln = La (4), Nd (5), Gd (6), Sm (7), Eu (8), Tb (9), Dy (10), Ho (11), Yb (12), Lu (13)) were successfully synthesized via transmetalation between 2,6-(2,6-C2H3-R2N=CH)(2)-C6H3Li and LnCl(3)(THF)(1 similar to 3.5). These complexes are isostructural monomers with two coordinating THF molecules, where the pincer ligand coordinates to the central metal ion in a kappa C:kappa N: kappa N' tridentate mode, adopting a meridional geometry.

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Novel water resistant sulfonated poly[bis(benzimidazobenzisoquinolinones)] (SPBIBIs) were synthesized from 6,6'-disulfonic-4,4'-binaphthy]-1,1',8,8'-tetracarboxylic dianhydride (SBTDA) and various aromatic ether tetraamines. The resulting polymers with IEC in the range of 2.17-2.87 mequiv g(-1) have a combination of desired properties such as high solubility in common organic solvents, film-forming ability, and excellent thermal and mechanical properties. Flexible and tough membranes, obtained by casting from m-cresol solution, had tensile strength, elongation at break, and tensile modulus values in the range of 87.6-98.4 MPa, 35.8-52.8%, and 0.94-1.07 GPa. SPBIBI membranes with a high degree of sulfonation displayed high proton conductivity and a good resistance to water swelling as well. SPBIBI-b with IEC of 2.80 mequiv g(-1) displayed the conductivity of 1.74 x 10(-1) S cm(-1) at 100 degrees C, which was comparable to that of Nafion (R) 117 (1.78 x 10(-1) S cm(-1), at 100 degrees C).

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The reaction of NdCl3 with 2 equiv. of Na-(BuC5H4)-C-t in THF(tetrahydrofuran) gives blue crystals [((BUC5H4)-C-t)(2)NdCl](2), C36H52Cl2Nd2(M-r = 844.11) Which crystallizes in the triclinic system with space group r bar>. The crystal data are a=11.978 (1), b=12.671(4), c=12.706(2)Angstrom, alpha=105.47(2), beta=99.38(1)? gamma=93.15 (2)degrees, V=1825 (3) Angstrom(3), Z = 2 , D-c = 1.53g/cm(3), F(000) = 450 , T = 298K , lambda(MoK alpha) = 0.71069 Angstrom, , mu = 14.97cm(-1). Final R = 0.0390, R-w = 0.0376 for 4329 reflections with I greater than or equal to 3 sigma(I-o). The molecule has a dimer structure with two certrosymmetrical chlorine bridges. The structural trend of these analogous complexes is discussed.

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The photo-induced decarbonylation of Cp'Cr(NO)(CO)(2) (1a) in MeCN solution in the presence of R2E2 (E = S, Se; R = Me, Ph) leads to the formation of chalcogenolato-bridged binuclear complexes Cp-2'Cr-2(NO)(2)(mu -ER)(2) [E = S; R = Me (2a), Ph (3a); E = Se, R = Me (4a), Ph (5a)] while reactions between Cp'M(NO)(CO)(2) [M = Mo (1b), W (1c)] and Ph2E2 (E = S, Se) result in mononuclear complexes Cp'M(NO)(EPh)(2) [M = Mo; E = S (9b), Se (10b); M = W, E = S (11c), Se (12c)]. The corresponding reactions of (1b) with Me2E2 (E = S, Se) yielded both mono and binuclear complexes: Cp'Mo(NO)(SeMe)(2) (8b), Cp-2'Mo-2(NO)(2)(mu -EMe)(2) [E = S (6b), Se (7b)]. The new complexes have been characterized by i.r., H-1-, C-13-n.m.r. spectra and by electron-impact mass spectrometry.

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The first mononuclear tungsten-citrato complex, (NH4)(3)[Li(H2O)(3)WO3(C6H4O7)] (1) has been prepared by the reaction of ammonium tetrathio tungstate and lithium citrate in CH3OH - H2O solution at pH 8.2. There are two crystallographically independent anions in the asymmetric crystallographic unit. The crystal structure of the title compound (triclinic, space group P (1) over bar, a = 6.901(1), b = 15.136(3), c = 16.107(3) Angstrom, alpha = 75.85(3), beta = 89.89(3), gamma = 89.97(3), V = 1631.4(6) Angstrom (3), R = 0.068, R-w = 0.1674 for 3878 reflections with I > 2 sigma (1)), reveals that in the compound a tungsten atom is coordinated to a fully deprotonated citrate as a tridentate ligand and three terminal oxygen atoms to form a distorted coordination octahedron.

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The reaction of [Cp*RhCl2](2) 1 with dilithium 1,2-dicarba-closo-dodecaborane(12)-1,2-dithiolate (a) and -diselenolate (b) afforded the 16-electron rhodium(III) half-sandwich complexes Cp*Rh[E2C2(B10H10)] [E=S (3a), Se (3b)]. The 18-electron trimethylphosphane rhodium(III) half-sandwiches Cp*Rh(PMe3)[E2C2(B10H10)] 4a-c were prepared from the reaction of Cp*RhCl2(PMe3) 2 with the same dichalcogenolates, including the ditelluride (c). The complexes 4a,b could also be obtained from the reaction of 3a,b with trimethylphosphane. The molecular geometry of 4b was determined by X-ray structural analysis. The 16-electron complexes 3 an monomeric in solution as shown by multinuclear magnetic resonance (H-1-, B-11-, C-13-, P-31- Se-77-, Rh-103-, Te-125-NMR). also in comparison with the data for the trimethylphosphane analogues 4a-c and for 6a in which the rhodium bears the eta(5)-1,3-C5H3 Bu-t(2) ligand. The Rh-103 nuclear shielding is reduced by 831 ppm (3a) and 1114 ppm (3b) with respect to the 18-electron complexes 4a,b. Similarly, the Se-77 nuclear shielding in 3b is reduced by 676.4 ppm with respect to that in 4b. (C) 1999 Elsevier Science S.A. All rights reserved.

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[PrAl (CF3COO)(2) (CF3CHOO) (C2H5)(2) (C4H8O)(2)](2) M-r = 1420. 56, monoclinic, P2(1)/n, a = 10. 651 (6) , b = 24. 276(9), c = 11. 110(5) Angstrom, beta = 107. 650 (4)degrees , V = 2737. 4(1) Angstrom (3) , Z = 2, D-c = 3. 45 g/cm(3) , F(000) = 2816 , T = 233K, MoK alpha radiation (lambda= 0. 71069 Angstrom), mu(MoK alpha) = 38. 017 cm(-1) , R = 0. 048 for 2847 observed reflections (I greater than or equal to 3 sigma(I)). It is isostructural with [LnAl (CF3COO)(2) (CF3CHOO) -R-2 (C4H8O)(2)](2) (Ln = Ho, R = Et; Ln = Ndt Y, R = Bu-1). Pr3+ is coordinated by eight oxygen atoms from five bridging ligands and two THF forming a distorted bicap-prism.

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Thirteen title complexes ROCOCH2CH2SnCl3 . L(R = C(1 similar to 5)alkyl;L = DBSO,HMPA) were synthesized and characterized by elemental analysis, IR,H-1 NMR. The crystal structure of n -PrOCOCH2CH2SnCl3 . DBSO was determined by the X-ray diffraction analysis. The crystal belongs to orthorhombic system,space group P2(1)2(1)2(1) with a = 1.062, b = 1.427, c = 1.635nm; Z = 4. The complex exists as a discrete molecule, and the tin atom attains a distorted octahedral geometry via the coordination of intramolecular carbonyl oxygen and the Lewis base donor atom. The transesterification of CH3OCOCH2CH2SnCl3 . L with alcohol was studied, and the intramolecular Lewis acid catalytic mechanism was suggested.

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合成了13个标题化合物POCOCH_2CH_2SnCl_3·L(R=C_(1~5)烷基;L=DBSO,HMPA),通过元素分析、IR和~1H NMR进行了表征.n-PrOCOCH_2CH_2SnCl_3·DBSO的晶体结构分析表明,该晶体属正交晶系;空间群P2_12_12_1;a=1.062,b=1.427,c=1.635nm;Z=4.该化合物为含有分子内碳基配位和Lewis碱配体配位的具有畸变八面体构型的单分子有机锡化合物.研究了CH_3OCOCH_2CH_2SnCl_3·L和醇的酯交换反应,提出了分子内Lewis酸催化的反应机理.

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The reactions of [Cp2Mo2(CO)4] (1) with 2,2'-dipyridyl disulphide (C5H4NS-)2, 8,8'-diquinolyl disulphide (C9H6NS-)2 and tetramethyl thiuram disulphide (Me2NC(S)S-)2 in toluene solution resulted in the cleavage of the Mo-Mo triple bond to yield molybdenum complexes [CpMo(CO)2(C5H4NS)] (2), [CpMo(CO)2(C9H6NS)] (3) and [CpMo(CO)2(S2CNMe2)] (4), respectively. The molecular structures of 2, 3 . O=PPh3 and 4 were determined by X-ray diffraction studies. Crystals of 2 are monoclinic, space group P2(1)/n, with Z = 4, in a unit cell of dimensions a = 6.448(1), b = 12.616(2), c = 14.772(2) angstrom, beta = 92.85(1)-degrees. The structure was refined to R = 0.028 and R(w) = 0.039 for 1357 observed reflections. Crystals of 3 . O=PPh3 are triclinic, space group P1BAR, with Z = 2, in a unit cell of dimensions a = 11.351(3), b = 13.409(3), c = 9.895(2) angstrom, alpha = 94.59(2), beta = 90.35(2), gamma = 78.07(2)-degrees. The structure was refined to R = 0.033 and R(w) = 0.037 for 3260 observed reflections. Crystals of 4 are monoclinic, space group P2(1)/a and Z = 4 with a = 12.468(5), b = 7.637(2), c = 13.135(4) angstrom, beta = 96.62(3). The structure was refined to R = 0.032 and R(w) = 0.042 for 1698 observed reflections. Each of complexes 2-4 contains a cyclopentadienyl ligand, a cis pair of carbonyls and a chelate ligand (S,N donor or S,S donor). All the compounds have distorted square-pyramid structures.

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catena-Poly[{pentaaqua(L-proline-O)-erbium-mu-(L-proline-O:O')} trichloride], {[Er(C5H9-NO2)2(H2O)5]Cl3}n, M(r) = 594.0, monoclinic, P2(1), a = 8.294 (1), b = 10.981 (3), c = 11.934 (3) angstrom, beta = 107.04 (2)degrees, V = 1039.2 (4) angstrom3, Z = 2, D(x) = 1.90 g cm-3, lambda(Mo Kalpha) = 0.71069 angstrom, mu = 45.2 cm-1, F(000) = 586, T = 298 K, R = 0.0244 for 1711 unique reflections [I > 3 sigma(I(o))]. The crystal consists of one-dimensional chains of infinite length in which one L-proline ligand bridges two neighboring Er ions, the other L-proline ligand being monodentate.

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合成了[NH_3(CH_2)_(10)NH_3]ZnCl_4配合物(简称DDAZn),用X射线衍射法研究了它的晶体结构,晶体属三斜晶系,空间群为P1,晶胞参数为:α=0.7296(1),b=1.0110(3),c=1.2814(4)nm;α=90.84(2),β=101.17(2),γ=92.52(2)°;Z=2.该配合物为层型结构.由单个四面体阴离子ZnCl_4~(2-)构成的阴离子层被夹在烷基铵阳离子层之间,形成“夹心面包”型体系.在层之间的烷基铵链在垂直于层的方向上倾斜排列.

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本文主要阐述运用稳定加液-反应系统,在实验室环境下模拟海水中方解石和文石形成时微量元素共沉淀现象,主要研究微量元素固-液体系中的迁移、转化和分配。进而在对其定量描述的前提下,研究各靶元素的共沉淀行为对各种反应条件的响应,从中提取出可以用于古海洋研究的替代性指标。所研究的微量元素和部分常量元素包括非金属元素硼和砷、碱土金属元素镁、过渡金属元素(锰、钴、镍、铜、和镉)、铀系元素(铀、钍和铅)以及钇和稀土元素。 本实验首先运用pH测试、高精度滴定分析等手段测定了实验的一些基本参数,如[H+]、碱度和[Ca2+],根据计算获得了各碳酸体系要素,并以此为基础建立了5℃、15℃和25℃及pCO2=0.0015 atm.=0.0030atm.下的人工海水中方解石或文石的沉淀动力学方程。研究表明: 1)在各个条件下,方解石或文石的沉淀速率(R)和其在海水中过饱和度(Ω)存在很好的相关性,可基本表达为Log R=k*Log(Ω-1)+b; 2) pCO2对会严重改变海水中的碳酸钙过饱和度,进而影响相应的沉淀速率,但对方解石或文石的沉淀动力学方程没有明显影响; 3)不同温度下所得的方解石或文石各自的沉淀动力学方程存在明显差异,表明这一过程受热力学元素控制。 在方解石和文石沉淀实验中,通过人为添加各种微量元素对它们的共沉淀行为进行模拟。首先通过直接溶解稀释法结合ICP-MS或采用离线螯合系统前处理结合ICP-MS测定海水、固体样品中各靶元素的浓度。在此基础之上通过换算得出各靶元素在海水([Me]sol’n)和方解石或文石沉淀([XMe]overg)中的含量,然后 计算出单个实验中各靶元素介于碳酸钙沉淀和海水之间的分异系数。 实验中通过改变晶核类型(方解石和文石)、温度、pCO2、碳酸钙过饱和度(2-12,以方解石计)、沉淀速率和靶元素起始浓度等参数,得到在不同反应条件下各靶元素的分异系数。基于分异系数之间的差异,各靶元素在方解石和文石沉淀过程中的共沉淀行为被加以分类和界定。在方解石中Mn、Co、Ni、Pb、Th、Cd、Cu、Mg等表现为相容元素。而在文石中Mn、Co、Ni、Cd等都属不相容元素。B、As、U与其他金属离子不同的是这三种元素是以BO33-、AsO33-、UO22+等基团的形式参予共沉淀的,其中BO33-和AsO33-是替代CO32-而UO22+取代Ca2+。 进一步总结各靶元素和反应条件的关系,初步得出碳酸钙沉淀动力学机制、温度、离子半径、碳酸钙矿物的晶格结构、溶液化学组成及其变化是影响微量元素随方解石和文石共沉淀过程的重要因素,并对各靶元素共沉淀模式进行了探讨。最后我们结合实际工作主要是文献中报导的有孔虫、珊瑚等生物钙质壳体或骨架中各靶元素的结果,对比我们的实验从中提取出了一些可应用于古海洋研究的潜在替代性指标,如: 1) 海水中CO32-浓度代用指标——文石U/Ca、Cd/Ca比,方解石U/Ca比; 2) 海水pH 代用指标——文石B/Ca、As/Ca 比; 3) 氧化还原代用指标——方解石Mn/Ca 比; 4) 海水化学代用指标——方解石Co/Ca 比、U/Ca 比文石Cu/Ca、Pb/Ca 比。 5)稀土元素代用指标——方解石质载体中的YREE/Ca比。 还有几种元素组合也非常具有价值,如Mn-Co-Ni 组合、B-U 组合。此外指出了现有微量元素古海洋指标应用过程中被忽略了的一些关键性因素,如文石Mg/Ca比受到文石沉淀速率的限制、方解石Cd/Ca 比受到沉淀速率和温度的双重影响等。

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本文主要运用稳定加液-反应系统对海水中方解石和文石形成时稀土元素的共沉淀现象进行了分析,研究了稀土元素在固-液体系中的迁移、转化和分配。进而在对其定量描述的前提下,研究了稀土元素共沉淀对各种反应条件的响应,并对共沉淀行为的机制进行了探讨。 本实验首先运用pH测试、高精度滴定分析等手段测定了实验中的一些基本参数,如[H+]、碱度和[Ca2+],根据计算结果获得了各碳酸体系要素,并以此为基础建立了5℃、15℃和25℃及pCO2=0.003atm下海水中方解石或文石的沉淀动力学方程。实验结果表明: 1)在各条件下,方解石或文石的沉淀速率(R)和其在海水中过饱和度(Ω)存在很好的线性相关性,即海相碳酸盐的沉淀动力学方程可以通过下面的基本表达式来表示:LogR=k*Log(Ω-1)+b ; 2)过高的稀土元素浓度会对文石或方解石的沉淀产生抑制作用,进而对共沉淀过程中YREEs的分异和分馏产生一定的影响。相比方解石而言,文石的沉淀动力学过程承受稀土元素的干扰能力更强; 3)不同温度下得到的方解石或文石各自的沉淀动力学方程存在明显的差异,表明这一过程受热力学因素控制。相对于方解石而言,温度对文石的沉淀动力学的影响更为显著。 与前人研究不同的是,本实验中YREEs的浓度设定在非常低的范围内,从而避免了过高浓度YREEs对方解石或文石沉淀动力学过程的干扰。在最终的反应液中,各种实验条件非常接近自然环境。有关稀土元素的共沉淀行为主要得出以下定性或定量化结论: 1)YREEs在随方解石或文石的共沉淀过程中,均发生了强烈的分异作用。在方解石实验中,稀土元素的分异系数分布曲线呈凸状分布;而在文石实验中,稀土元素的分异系数随原子序数的增加逐渐减小,遵循镧系收缩的规律。总的来说,稀土元素,尤其轻稀土元素在文石中的分异作用要强于方解石。 2)无论是方解石还是文石,沉淀速率对YREEs的分异作用都有着明显的影响。在方解石中,YREEs的分异系数随沉淀速率的增加呈一致性递减趋势;而在文石中,其分异系数对文石沉淀速率有着截然不同的响应:轻稀土元素(La, Ce, Nd, Sm, Eu, Gd)的分异系数随文石沉淀速率的增加而下降,而重稀土元素(Ho, Y, Tm, Yb , Lu)的分异系数则随文石沉淀速率的增加呈上升趋势。 3)在方解石中YREEs的分异系数之间存在非常好的相互关系,表明这些元素是以成比例的方式参与共沉淀。整个谱系呈现中等强度的分馏,MREE相对于LREE和HREE要更为富集;在文石中由于沉淀速率的作用不同,只有Y、Ho、Yb、Lu等元素的分异系数之间有较好的相互关系。YREEs出现了差异性的强烈分馏,在新生成沉淀中轻稀土元素相对于重稀土元素强烈富集。 4)YREEs在溶液中和碳酸盐晶体表面的碳酸根配位形式对YREEs在共沉淀过程中的分异作用极为重要,YREEs在碳酸盐晶体表面的吸附是整个谱系发生分馏效应的关键环节。对于文石来讲,晶体中有效YREE离子和Ca离子半价大小之间的相近程度是其分馏效应的关键因素;而对于方解石来说,YREEs在方解石晶格中的安置就是其分馏效应的关键控制因子,但在晶格安置中起到关键作用的是YREEs和方解石中O原子之间离子键M-O的键长,而非离子半径。 5)综合YREEs在方解石中的分异作用和分馏效应,我们认为M2(CO3)3-CaCO3和MNa(CO3)2-CaCO3是最为可能的两种固体溶液形成模式。 最为重要的是,对比我们的实验结果与前人在灰岩、叠层石、微生物成因碳酸盐等方解石质载体中的研究成果,两者之间出现了非常好的一致性。我们认为方解石质载体将是重建古海水中稀土元素相关信息的重要工具。相比之下,文石质载体不适合作为类似的载体。