Operator and organizational maintenance manual for TOW Weapon System guided missile system M220A1 (1440-00-169-1764) : TOW heavy antitank/assault weapon system.

"January 1980."

Organizational maintenance manual for gun, air defense artillery, self-propelled, 20-mm, M163A2, cannon M168, mount M157A2, sight M61A1 and radar AN/VPS-2A, (NSN 2350-01-169-2833).

Includes index.

DS, GS, and depot maintenance manual : maintenance kit MK-1035/ARC-131, (NSN 5821-00-935-0058).

Includes index.

Alaska employment security act as amended, chapter five, First extraordinary session laws of Alaska 1955, as amended by chapter 62, 75 and 169, Session laws of Alaska, 1957; chapter 46, 64 and 97, Session laws of Alaska, 1959 and chapter 60, Session laws of Alaska, 1960.

Mode of access: Internet.

In Equity no. 169. In the District Court of the United States for the Northern District of California : the Equitable Trust Company of New York, as Trustee, Complainant, against Western Pacific Railway Company, Chester L. Hovey, as Receiver of Boca and Loyalton Railroad Company, and Mercantile Trust Company of San Francisco, as Trustee, Defendants, and Central Trust Company of New York, as Trustee, Intervening Defendant and Cross-complainant.

[V.1.] Proceedings on Master's sale -- [v.2.] Decree of forclosure and sale -- [v.3.] Ancillary decree of foreclosure and sale.

Fragm. lat. III 8 - Digestum novum (De regulis iuris D.50.17.65 - 117; 158 - 169; 171 - 192)

Trägerbände: Ms. Barth. 52; Ms. Barth. 66; Vorbesitzer: St. Peter Urach; Bartholomaeusstift Frankfurt am Main

Na 1 Nachlass Max Horkheimer, 561 - Korrespondenzen mit Leo Löwenthal (p. VI 26, 1-169)

79 Briefe zwischen Max Horkheimer und Leo Löwenthal; 1 Brief von Leo Löwenthal an Everett C.Hughes, 31.05.1956; 1 Brief von Max Horkheimer an E. Henne, 06.02.1956; 1 Brief von Ralph W. Tyler an Leo Löwenthal, 06.02.1956;

Dark matter in dwarf irregular galaxies, DDO 210 and DDO 169

It has been proposed that dwarf irregular galaxies can be separated into two classes based on their formation mechanism; that they are the result of the collapse of a primordial gas cloud or that they are the product of condensation of gas in the tidal tails of interacting galaxies. Simulations of galaxy interactions indicate that one can differentiate between these two scenarios by the dark matter content, with a low dark matter content indicating a fossil tidal dwarf. The purpose of this dissertation was to explore the dark matter distribution of two dwarf irregular galaxies using optical and neutral atomic hydrogen data. For DDO 210, the method of mass-modelling was used to determine its dark matter. About 64% of the galaxy mass was calculated to be in the form of dark matter and hence it is unlikely to be a fossil tidal dwarf. The method of mass-modelling could not be used for DDO 169 as the galaxy shows evidence of being tidally disrupted and hence, has a disturbed velocity field. Instead, the suggestion that dark matter might be responsible for a pressure anomaly in DDO 169 was tested to determine its dark matter content. According to this method, a pressure anomaly does exist but without a concrete value for the scale-height, it is unclear whether the anomaly is due to the presence of dark matter. Hence one cannot say how much dark matter might actually be present in DDO 169. A rotation curve would be required to do this. ^

Concentrations of chemical elements in bottom sediments from the Southeast Pacific

Data from the Appendix to the PhD Thesis of the author.

(Table 1) Phosphorus and carbon chemistry of ODP Holes 169-1033B and 169-1034B

Uncertainty currently exists about the removal of carbon (C) and phosphorus (P) from the oceanic reservoir, especially in low oxygen settings. In this paper, the cycling of C and P is examined in sediments from the anoxic Saanich Inlet, cored by Ocean Drilling Program (ODP) Leg 169S in 1996 at two sites. Although Corg/Porg ratios are high and increase with depth in the Saanich Inlet, this effect is due largely to a remobilization of P from an organic matter sink to an authigenic sink. Reducible sedimentary components act as temporary shuttles in this process even in this anoxic setting, with the ultimate burial sink for the remobilized P being carbonate fluorapatite. The effective Corg/Preactive molar ratio appears to be about 150-200, indicating some preferential loss of P compared to C during organic matter degradation, but not approaching previously reported values of over 3000 in black shales. Reactive P accumulation rates in this basin range from 10,000-60,000 µmol/cm**2/kyr, greatly exceeding the range of 500-8000 µmol/cm**2/kyr found in most continental-margin settings, including regions of modern phosphogenesis. The initiation of marine sedimentation in the Saanich Inlet occurred after deglaciation, and the high rates of P burial seen here may provide an end-member example of the effects of sea level and margin sedimentation on the distribution of P within the marine P cycle.