Costs - UCPR rr 681 and 684

In BHP Coal Pty Ltd v K Orenstein & Koppel AG (No 2) [2009] QSC 64 McMurdo J considered the circumstances in which the ordinary rule under r 681 of the Uniform Civil Procedure Rules 1999 (Qld) (UCPR) that costs should follow the event should be departed from in favour of a party who was unsuccessful overall, but who succeeded on particular questions. When the court is satisfied that a departure from the usual order under r 681 of the UCPR is justified, it appears increasingly willing to exercise the power in r 684(2) to declare what percentage of costs was applicable to a particular issue

破甲机理的力学分析及简化模型(681破甲机理课题进展报告)

<正>引言681课题破甲机理组,几年来在参加单位大力协同下,特别在实验研究方面,取得了许多成果,使我们对破甲过程的认识有了实质性的提高。破甲机理研究的任务和目的是,通过实验和分析的手段,弄清楚破甲过程以及影响这个过程的靶板方面和射流方面的主要因素,建立定量关系和可靠、实用的计算公式,为新型装甲材料和装甲板的研制,为提高破甲弹威力提供依据。本报告的目的是汇报1974年、1975年我们在破甲机理力学分析和简化计算模型方面

Na 50 Nachlass Arthur Schopenhauer - 'Schopenhauer-Archiv', 681 - Mitteilungen zu den finanziellen Forderungen gegenüber dem Bankhaus Muhl

abgedruckt in: Schopenhauer-Jahrbuch 56 (1975), S 169

Na 1 Nachlass Max Horkheimer, 681 - "Antisemitism anong American Labor" Band IV (p. IX 146.1 Bd. IV)

"Antisemitism among Amercan Labor. Report on a Research Project conducted by the Institute of Soial Research in 1944-1945". Typoskript, in 4 Bänden gebunden, 1450 Blatt;

Benoît Peeters, Derrida. Buenos Aires, Fondo de Cultura Económica, 2013, 681 páginas

Fil: Mallol, Anahí Diana. Universidad Nacional de La Plata. Facultad de Humanidades y Ciencias de la Educación; Argentina.

Benoît Peeters, Derrida. Buenos Aires, Fondo de Cultura Económica, 2013, 681 páginas

Fil: Mallol, Anahí Diana. Universidad Nacional de La Plata. Facultad de Humanidades y Ciencias de la Educación; Argentina.

Amino acids and carbohydrates in sediments and interstitial waters of ODP Site 112-681

Total organic carbon (TOC), dissolved organic carbon (DOC), total hydrolyzable amino acids (THAA), amino sugars (THAS), and carbohydrates (THCHO) were measured in sediments and interstitial waters from Site 681 (ODP Leg 112). TOC concentrations vary between 0.75% and 8.2% by weight of dry sediment and exhibit a general decrease with depth. DOC concentrations range from 6.1 to 49.5 mg/L, but do not correlate with TOC concentrations in the sediment. Amino compounds (AA and AS) and sugars account for 0.5% to 8% and 0.5% to 3% of TOC, respectively, while amino compounds make up between 2% and 27% of total nitrogen. Dissolved hydrolyzable amino acids (free and combined) and amino sugars were found in concentrations from 3.7 to 150 µM and from 0.1 to 3.7 µM, respectively, and together account for an average of 8.5% of DOC. Dissolved hydrolyzable carbohydrates are in the range of 6 to 49 µM. Amino acid spectra are dominated by glycine, alanine, leucine, and phenylalanine; nonproteinaceous amino acids (gamma-amino butyric acid, beta-alanine, and ornithine) are enriched in the deeper part of the section, gamma-amino butyric acid and beta-alanine are thought to be indicators of continued microbial degradation of TOC. Glycine, serine, glutamic acid, alanine, aspartic acid, and ornithine are the dominating amino compounds in the pore waters. Spectra of carbohydrates in sediments are dominated by glucose, galactose, and mannose, while dissolved sugars are dominated by glucose and fructose. In contrast to the lack of correlation between abundances of bulk TOC and DOC in corresponding interstitial waters, amino compounds and sugars do show some correlation between sediments and pore waters: A depth increase of aspartic acid, serine, glycine, and glutamic acid in the pore waters is reflected in a decrease in the sediment, while an enrichment in valine, iso-leucine, leucine, and phenylalanine in the sediment is mirrored by a decrease in the interstitial waters. The distribution of individual hexoseamines appears to be related to zones of bacterial decomposition of organic matter. Low glucoseamine to galactoseamine ratios coincide with zones of sulfate depletion in the interstitial waters.