Organizational maintenance repair parts and special tools lists : grader, road, motorized, heavy duty, DED NSN 3805-00-155-7093, Huber Corporation model F1500MW and NSN 3805-01-064-3878, Huber Corporation model F1500M.

Includes indexes.

Direct support and general support maintenance manual : grader, road, motorized, heavy duty, DED, Huber Corporation models F1500M (3805-00-155-7093), F1500MW (3805-01-064-3878).

Includes index.

Operator and organizational maintenance manual : grader, road, motorized, heavy duty, DED Huber Corporation models F1500M (3805-00-155-7093), F1500MW (3805-01-064-3878).

Includes indexes.

Operator, organizational and direct support maintenance manual : tentage for Hawk Missile System ... cover, Hawk Missile FSN 8340-064-5050.

Includes index.

Organizational and direct support maintenance repair parts and special tools list : tentage for Hawk Missile equipment, tent, frame type, maintenance, 32 ft by 20 ft (FSN 8340-951-6419) ... cover, Hawk Missile (FSN 8340-064-5059).

Includes index.

Operator's and organizational maintenance manual : doppler navigation set AN/ASN-128 (NSN 5841-01-064-9738).

"May 1979."

Operator's and organizational maintenance manual : test set, radio data link, sound ranging, TS-3566/GRA-114 (NSN 5895-01-064-9740).

"30 July 1982."

Operator's, organizational, direct support, and general support maintenance manual : power supply PP-7662/U (NSN 4940-01-064-7342).

"November 1979."

Operator's, organizational, direct support, and general support maintenance manual : test set, relay TS-1775/U, NSN 6625-00-064-6096.

"October 1975."

Operator, organizational, DS, GS, and depot maintenance manual including repair parts and special tool lists : test set, electronic system AN/ASM-338.

"March 1968."

Measurement and correlation of the solubility of telmisartan (form A) in nine different solvents from 277.85 to 338.35 K

The solubility of telmisartan (form A) in nine organic solvents (chloroform, dichloromethane, ethanol, toluene, benzene, 2-propanol, ethyl acetate, methanol and acetone) was determined by a laser monitoring technique at temperatures from 277.85 to 338.35 K. The solubility of telmisartan (form A) in all of the nine solvents increased with temperature as did the rates at which the solubility increased except in chloroform and dichloromethane. The mole fraction solubility in chloroform is higher than that in dichloromethane, which are both one order of magnitude higher than those in the other seven solvents at the experimental temperatures. The solubility data were correlated with the modified Apelblat equation and λh equations. The results show that the λh equation is in better agreement with the experimental data than the Apelblat equation. The relative root mean square deviations (σ) of the λh equation are in the range from 0.004 to 0.45 %. The dissolution enthalpies, entropies and Gibbs energies of telmisartan in these solvents were estimated by the Van’t Hoff equation and the Gibbs equation. The melting point and the fusion enthalpy of telmisartan were determined by differential scanning calorimetry.

Global compilation of benthic data sets I

Approaches to quantify the organic carbon accumulation on a global scale generally do not consider the small-scale variability of sedimentary and oceanographic boundary conditions along continental margins. In this study, we present a new approach to regionalize the total organic carbon (TOC) content in surface sediments (<5 cm sediment depth). It is based on a compilation of more than 5500 single measurements from various sources. Global TOC distribution was determined by the application of a combined qualitative and quantitative-geostatistical method. Overall, 33 benthic TOC-based provinces were defined and used to process the global distribution pattern of the TOC content in surface sediments in a 1°x1° grid resolution. Regional dependencies of data points within each single province are expressed by modeled semi-variograms. Measured and estimated TOC values show good correlation, emphasizing the reasonable applicability of the method. The accumulation of organic carbon in marine surface sediments is a key parameter in the control of mineralization processes and the material exchange between the sediment and the ocean water. Our approach will help to improve global budgets of nutrient and carbon cycles.