Synthesis and Metal-ion Binding Properties of New N2S4O2- and N2S5O2-Donor Macrocycles

Synthetic procedures for new mixed-donor macrocycle compounds were reported. The macrocyclic compounds were used in solvent extraction metal picrates such as Ag+, Hg2+, Cd2+, Zn2+, Cu2+, Ni2+, Mn2+, Pb2+, and Co2+. The metal picrate extractions were investigated at 25±0.1°C with the aid of UV-visible spectrometry. It was found that 6,7,9,10,12,13,23,24-octahydro-19H,26Hdibenzo[h,t](1,4,7,13,16,22,10,19) dioxatetrathiadiazasiclotetracosine-20,27(21H,28H)-dione showed selectivity towards Ag+, Hg2+, and Cd2+ among the other metals. The extraction constants (Log Kex) and complex compositions were determined for the Ag+ and Hg2+ complexes for this compound and 9,10,12,13,23,24,26,27,29,30-decahydro-5H,15H-dibenzo-[h,w][1,4,7,13,16,19,25-,10,22] dioxapentathiadiazacycloheptacosine-6,16(7H,17H)-dione.

Preparation and the investigation of its electrochemical and photoluminescent characteristics of organic-inorganic hybrid multilayers containing europium-substituted heteropolytung state

Photoluminescent multilayers were fabricated by layer-by-layer deposition between europium-substituted heteropolytungstate K-13 [Eu(SiW11O39)(2)].28H(2)O (denoted ESW) and a cationic polymer of quaternized poly(4-vinylpyridine) partially complexed with osmium bis(2,2'-bipyridine) (denoted as QPVP-Os) on glassy carbon and quartz substrates. The resulting photoluminescent organic-inorganic hybrid multilayers were characterized by electrochemical impedance spectroscopy, UV-Vis absorption spectrometry, cyclic voltammetry and photoluminescence spectra. Electrochemical impedance spectroscopy, UV-Vis absorption spectrometry and cyclic voltammetry results demonstrated that the multilayers were regular growth each layer adsorption. The photoluminescent properties of the films at room temperature were investigated to show the characteristic Eu3+ emission pattern of D-5(0) --> (7) F-j.

Bestimmung des Kostenverlaufs von Molkereiabteilungen in Abhängigkeit von der Kapazitätsgröße und -auslastung. IV. Teil: H-Milch-Abteilung

Es werden die Kosten der H-Milchabteilung bei drei verschiedenen Kapazitätsgrößen mit jeweils variierter Kapazitätsauslastung nach einer speziellen Form der Teilkosten­rechnung bestimmt. Die Kapazitätsgrößen betragen 3300, 6600 und 9900 1-l-Packungen pro Stunde. Im Jahr werden zwi­schen 2,9 und 53,6 Mio. Einheiten hergestellt; dabei variie­ren die Stückkosten zwischen 30,65 und 18,85 Pf/1-l-Packung. Es zeigt sich dabei, daß die Kostendegression entscheidend stärker durch den Grad der Kapazitätsauslastung als durch die Kapazitätsgröße beeinflußt wird.

Cinética da maturação nuclear in vitro de oócitos bubalinos

Com o objetivo de avaliar a cinética da maturação in vitro de oócitos bubalinos, foram cultivados 1.619 oócitos com cumulus oophorus compacto em quatro diferentes tratamentos: T1 - TCM 199 com 10% de Soro Fetal Bovino (SFB) (meio base); T2 - Meio base e células da granulosa (CG); T3 - Meio base, CG, 10 UI de gonadotrofina coriônica equina (eCG) e 10 UI de gonadotrofina coriônica humana (hCG); T4 - Meio base, 10 UI de eCG, 10UI de hCG e 1 µg de 17b-estradiol / ml, em tempos de 14 a 17h, 20 a 22h, 23 a 25h, 26 a 28h, 29h e 32h de cultivo em estufa de CO₂ a 5% e temperatura de 38,5ºC. No tratamento 1, observou-se que 81,83%, 69,61%, 65,88%, 60,28%, 64,98% e 67,67% dos ovócitos reiniciaram a meiose. No tratamento 2, as taxas de reinicio da meiose foram de 76,06%, 72,06%, 69,78%, 68,12%,74,97% e 89,96%, no tratamento 3 estes percentuais foram de 83,59%, 78,86%, 77,49%, 82,4%, 72,92% e 81,06% e com o tratamento 4 os índices foram de 95,0%, 91,82%, 93, 17%, 91,65%, 92,09% e 74,99% nos tempos de 14 a 17h, 20 a 22h, 23 a 25h, 26 a 28h, 29h e 32h de cultivo, respectivamente, podendo-se concluir que o meio com maior suplementação proporciona maior taxa de reinício da meiose em menor tempo, assim como o aumento no tempo de cultivo pode levar a maiores índices de degeneração.

Sand fraction, carbonate and organic carbon contents of ODP Hole 175-1085A

Site 1085 is located on the continental rise of southwest Africa at a water depth of 1713 m off the mouth of the Orange River in the Cape Basin. The site is part of the suite of locations drilled during Leg 175 on the Africa margin to reconstruct the onset and evolution of the elevated biological productivity associated with the Benguela Current upwelling system (Wefer, Berger, Richter, et al., 1998, doi:10.2973/odp.proc.ir.175.1998). Three sediment samples were collected per section from Cores 170-1085A-28H through 45X (251-419 mbsf) to provide a survey of the sediment record of paleoproductivity from the middle late Miocene to the early Pliocene (~8.7-4.7 Ma), which is a period that includes the postulated northward migration and intensification of the Benguela Current and the establishment of modern circulation off southwest Africa (Siesser, 1980; Diester-Haass et al., 1992; Berger et al., 1998). Core 170-1085A-30H (270-279 mbsf) had essentially no recovery; this coring gap was filled with samples from Cores 170-1085B-29H and 30H (261-280 mbsf). The results of measurements of multiple paleoproductivity proxies are summarized in this report. Included in these proxies are the radiolarian, foraminiferal, and echinoderm components of the sand-sized sediment fraction. Opal skeletons of radiolarians (no diatoms were found) relate to paleoproductivity and water mass chemistry (Summerhayes et al., 1995, doi:10.1016/0079-6611(95)00008-5; Lange and Berger, 1993, doi:10.2973/odp.proc.sr.130.011.1993; Nelson et al., 1995, doi:10.1029/95GB01070). The accumulation rates of benthic foraminifers are useful proxies for paleoproductivity (Herguera and Berger, 1991, doi:10.1130/0091-7613(1991)019<1173:PFBFAG>2.3.CO;2; Nees, 1997, doi:10.1016/S0031-0182(97)00012-6; Schmiedl and Mackensen, 1997, doi:10.1016/S0031-0182(96)00137-X) because these fauna subsist on organic matter exported from the photic zone. Echinoderms also depend mainly on food supply from the photic zone (Gooday and Turley, 1990), and their accumulation rates are an additional paleoproductivity proxy. Concentrations of calcium carbonate (CaCO3) and organic carbon in sediment samples are fundamental measures of paleoproductivity (e.g., Meyers, 1997, doi:10.1016/S0146-6380(97)00049-1). In addition, organic matter atomic carbon/nitrogen (C/N) ratios and delta13C values can be used to infer the origin of the organic matter contained within the sediments and to explore some of the factors affecting its preservation and accumulation (Meyers, 1994, doi:10.1016/0009-2541(94)90059-0).