范文正公集 20巻. 別集 4巻. 政府奏議 2巻. 尺牘 3巻. 年譜 1巻. 年譜補遺 1巻. 言行拾遺事錄. 4巻鄱陽遺事錄 1巻. 遺蹟 1巻. 建立義莊規矩 1巻. 褒賢集 5巻. 范文正公集補編 5巻. 范侍郎公遺文 1巻. 范忠宣公集 20巻. 奏議 2巻. 遺文 1巻. 附錄 1巻. 補編 1巻

Mode of access: Internet.

歷代地理志韻編今釋 20巻 坿校勘記 1巻. 皇朝輿地韻編 2巻 坿校勘記 1巻 坿地志韻編唐志補闕正誤考異 1巻. 歷代地理沿革圖 1巻. 曆代紀元編 3巻

Mode of access: Internet.

Operator's and organizational maintenance manual : water purification unit, van-type, body mounted, electric driven, AC, 115, 208 V, single- and 3-phase, 60 hertz, 1/20 to 2 hp, 3000 gph (MET-PRO model 3000V), NSN 4610-00-168-1799.

"18 June 1980."

Organizational maintenance repair parts and special tools lists : water purification unit, van-type, body mounted, electric driven, AC, 115/208 V, single and 3 phase, 60 hertz, 1/20 to 2 hp, 1500 GPH, model EMC-1500S, NSN 4610-01-037-8746.

"15 May 1980."

Direct support and general support maintenance manual : water purification unit, van type, body mounted, electric motor driven, AC, DC, 115, 208 V, single and 3 phase, 60 hertz, 1/20 to 2 hp, 1500 gph, model EMC-1500S, NSN 4610-01-037-8746, EMC Industries Inc., DAAKO1-76-C-5661.

"1 August 1979."

Direct support and general support maintenance repair parts and special tools lists (including depot maintenance repair parts and special tools) : water purification unit, van-type, body mounted, electric driven, AC, 115/208 V, single and 3 phase, 60 hertz, 1/20 to 2 hp, 1500 gph, model EMC-1500S, NSN 4610-01-037-8746.

"15 May 1980."

Direct support and general support maintenance repair parts and special tools list : water purification unit, van-type, body mounted, electric driven, AC 115/208V, single and 3-phase, 1/20 to 2 hp, 3000 gph (MET-PRO model 3000 V), NSN 4610-00-168-1799.

"10 February 1983."

Synthesis, crystal structure and properties of H-8[P4W14O58Na4 (H2O)(20)] center dot 16H(2)O

A novel heteropoly tungstophosphates, H-8[P4W14O58Na4(H2O)(20)] . 16H(2)O, was synthesized by hydrothermal method and characterized by elemental analysis, IR spectrum and single-crystal X-ray structure analysis. The thermal stability of the compound was investigated by using TG-DTA. The crystal is triclinic system with space group P (1) over bar, a = 1. 137 9(2) nm, b=1. 363 2(3) nm, c=1. 627 1(3) nm; alpha=78. 20(3)degrees, beta=71, 20(3)degrees, gamma= 71. 62(3)degrees; V = 2. 252 5(8) nm(3), Z=1, M-r= 4 374. 38, D-c = 3. 225 mg/cm(3), mu = 18. 007 mm(-1), F(000)=1 972, R=0. 074 2, R-w=0. 200 4. The result of structure analysis shows that the anion of the compound consists of two PW7O29Na2(H2O)(10) subunits and two linked phosphorous atoms. A kind of microporous with size of 0. 661 4 nm X 0. 318 9 nm was formed in the crystal structure.

Oxygen, hydrogen, and carbon isotopic compositions in deep sea cherts, porcellanites, and coexisting carbonates from DSDP Legs 2, 3, 6, 7, 11, 14, 16, 17, and 20

Seventy four samples of DSDP recovered cherts of Jurassic to Miocene age from varying locations, and 27 samples of on-land exposed cherts were analyzed for the isotopic composition of their oxygen and hydrogen. These studies were accompanied by mineralogical analyses and some isotopic analyses of the coexisting carbonates. d18O of chert ranges between 27 and 39%. relative to SMOW, d18O of porcellanite - between 30 and 42%. The consistent enrichment of opal-CT in porcellanites in 18O with respect to coexisting microcrystalline quartz in chert is probably a reflection of a different temperature (depth) of diagenesis of the two phases. d18O of deep sea cherts generally decrease with increasing age, indicating an overall cpoling of the ocean bottom during the last 150 m.y. A comparison of this trend with that recorded by benthonic foraminifera (Douglas and Savin, 1975; http://www.deepseadrilling.org/32/volume/dsdp32_15.pdf) indicates the possibility of d18O in deep sea cherts not being frozen in until several tens of millions of years after deposition. Cherts of any Age show a spread of d18O values, increasing diagenesis being reflected in a lowering of d18O. Drusy quartz has the lowest d18O values. On-land exposed cherts are consistently depleted in 18O in comparison to their deep sea time equivalent cherts. Water extracted from deep sea cherts ranges between 0.5 and 1.4 wt %. dD of this water ranges between -78 and -95%. and is not a function of d18O of the cherts (or the temperature of their formation).

Aspectos da economia alimentar do Bronze Pleno da Beira Alta : a fauna de grandes mamíferos das «Salas 2 e 20» do Buraco da Moura de S. Romão (Seia)

Estuda-se a associação de grandes mamíferos recolhida em unidades estratigráficas das "Salas 20 e 2" do Buraco da Moura de S. Romão (Seia) correspondentes a uma ocupação do Bronze Pleno. Devido à natureza predominantemente ácida dos terrenos de toda a região beirã, restos faunísticos como os agora estudados são excepcionais. Tal facto valoriza as conclusões obtidas do seu estudo, não apenas sobre as bases de subsistência e hábitos alimentares, mas também acerca da economia das populações que, no Bronze Pleno, ocuparam a Bacia do Alto Mondego. Comprovou-se uma importante actividadepastoril, documentada pela predominância, no espectro faunístico, dos bovinos e ovinos e onde a caça ocupava um lugar muito secundário. Tal situação reforça a proposta de atribuição da degradação do coberto florestal da área serrana como tendo origem antrópica, datando talvez desde o IV milénio a. C., ligando-se á necessidade da obtenção de terras de pastoreio.