Na 1 Nachlass Max Horkheimer, 13 - Korrespondenzen u.a. mit Familie Eder (p. I 7, 1-223)

7 Briefe zwischen Edward Mead Earle, American Committee for International Studies, Princeton N. J. und Max Horkheimer, 1940-1941; 3 Briefe zwischen Margaret Ebert und Margot von Mendelssohn, 1941, 28.08.1941; 6 Briefe zwischen C. C. Eckhardt und Max Horkheimer, 1940; 5 Briefe zwischen Kay Eckstein und Max Horkheimer, 1940; 2 Briefe zwischen George Eckstein und Max Horkheimer, 16.05.1939, 35.05.1939; 1 Brief von F. K. Eden an Max Horkheimer, 02.04.1944; 33 Briefe zwischen Leopold Eder, Frieda Eder, Ruth Eder und Max Horkheimer, 1937-1940; 2 Briefe zwischen Dale Edwards und Max Horkheimer, 16.07.1940; 1 Brief von Hedwig Ehrlich an Max Horkheimer; 1 Brief von Max Horkheimer an Albert Einstein, 20.02.1935; 1 Brief von Max Horkheimer an W. Eisemann, 02.11.1939; 1 Brief von Else Eisner an Max Horkheimer, 09.12.1935; 2 Briefe zwischen Edit Elbogen und Max Horkheimer, 24.03.1942, 26.03.1942; 1 Brief von Käte von Hirsch an Max Horkheimer, 03.08.1941; 2 Briefe von Emmy Elbogen an Margot von Mendelssohn, 1945; 2 Briefe zwischen Paul Elbogen und Max Horkheimer, 02.06.1944, 09.06.1944; 4 Briefe zwischen Norbert Elias und Max Horkheimer, 1934-1935; 1 Brief von Werner B. Ellinger an Max Horkheimer, 16.12.1937; 19 Briefe zwischen dem Emergency Committee in Aid of Displaced Foreign Scholars New York und Max Horkheimer, 1938-1944; 2 Briefe zwischen dem Emergency Rescue Committee New York und Max Horkheimer, 12.06.1941, 14.06.1941; 1 Brief von F.L. Neumann an Emhardt, 13.02.1939; 23 Briefe zwischen Alice Engel und Max Horkheimer, 1937-1941; 9 briefe zwischen Paul Doernberg, Sofie Doernberg und Max Horkheimer, 1940-1942; 3 Briefe zwischen der Hebrew Sheltering and Immigrant Aid Society New York und Max Horkheimer, 05.01.1942, 1942; 1 Brief von der Selfhelp of Emigres from Central Europe, New York an Max Horkheimer, 18.08.1941; 2 Briefe zwischen R. Weissmann und Max Horkheimer, 09.01.1941, 03.02.1941; 5 Briefe zwischen Ernst Engelberg und Max Horkheimer, 1939-1940, 07.06.1939; 1 Brief von Fritz Epstein an Max Horkheimer, 10.04.1937; 1 Brief von Erika Ermel an Max Horkheimer, 15.09.1948; 2 Briefe zwischen Max Ernst und Max Horkheimer, 23.01.1936; 4 Briefe zwischen Margot Esser und Max Horkheimer, 1935-1936; 16 Briefe zwischen Rene Etiemble und Max Horkheimer, 1936-1938; 4 Briefe zwischen L.M. Ettlinger und Max Horkheimer, 1937; 8 Briefe zwischen Walter Fabien und Max Horkheimer, 1937-1941; 1 Brief von Max Horkheimer an Henry Pratt Fairchild, 25.03.1941; 2 Briefe zwischen Marvin Farber und Max Horkheimer, 14.03.1940, 17.05.1940; 4 Briefe zwischen Walter Farley udn Max Horkheimer, 1935, 01.10.1935; 8 Briefe zwischen Alexander Farquharson und Max Horkheimer, 1935-1939;

MS 073 Guide to the William C. Moloney MD papers; 1952-1954

William C. Moloney MD kept a personal journal, with photographs, for much of his two years in Japan with the Atomic Bomb Casualty Commission. In January of 1986, Dr.Moloney donated his journal, correspondence and diary pages to the Harris County Medical Archive. He died in 1998 at the age of 91. His first contribution was a set of ten reprints representing his work with the ABCC from 1952 to 1954. Dr.Moloney's journal is a fine document, one which will be of great use to historians. It is an important record of personal impressions, thoughts and details of events. The journal gives new insights into the work of the ABCC and into the people who participated in that work. Dr. Moloney wrote in his journal from April 1952 to February 1954. The Korean War was on and there was a great deal of military activity in southern Japan. The collection is open for research. The collection consists of a handwritten journal, loose calendar or notebook pages and some reprints. The journal is in generally fair condition. The paper is slightly acidic and the binding is loose. There are numerous photos glued onto the pages. The collection encompasses the years 1952-1954 and is 0.25 cubic feet (1 box).

Producción de cerezo en Mendoza : viabilidad técnico-económica, basada en un modelo de simulación

Se plantea el problema de la correlación existente entre la factibilidad técnico-económica del cultivo del cerezo y su ubicación en las diferentes zonas de cultivo en la Provincia de Mendoza. El objetivo es la determinación de las localizaciones más convenientes. Se ha observado el comportamiento del cultivo del cerezo, en un periodo de 15 años, en varias zonas de la Provincia de Mendoza, analizando los resultados desde un enfoque de aptitud ecológica y de evaluación económica. Para ello, se ha elaborado un modelo de simulación que abarca las principales variables ecológicas y los resultados económicos de precios y costos de cosecha. Resalta, en los resultados, la contradicción entre aptitudes ecológicas y económicas. En las zonas tradicionales de cultivo se obtienen mejores rendimientos por ha, pero el ingreso neto es menor que en las más templadas y precoces del Este de Mendoza, implantadas recientemente con nuevos cultivares, como Marvin Brooks, New Star, Gardner, Celeste y otros que logran, como primicias, precios mucho más altos en el mercado. Este resultado permite aconsejar a los productores sobre los lugares y los cultivares más convenientes para los nuevos cerezales.

Chemical and mineral compositions of basalts and volcanic glasses from DSDP Sites 65-483 and 65-485

Major and rare earth element (REE) data for basalts from Holes 483, 483B, and 485A of DSDP Leg 65, East Pacific Rise, mouth of the Gulf of California, support a simple fractional crystallization model for the genesis of rocks from this suite. The petrography and mineral chemistry (presented in detail elsewhere) provide no evidence for magma mixing, but rather a simple multistage cooling process. Based on its lowest TiO2 content (0.88%), FeO*/MgO ratio (0.95 with total Fe as FeO), and Mg# (100 Mg/Mg + Fe" = 70), sample 483-17-2-(78-83) has been selected as the most primitive primary magma of the samples analyzed. This is supported by the REE data which show this sample has the lowest total REE content, a La/Sm_cn (chondrite-normalized) = 0.36, and Eu/Sm_cn = 1.05. Because other samples analyzed have higher SiO2, lower Mg#, and a negative Eu anomaly (Eu/Sm_cn as low as 0.89), they are most likely derivative magmas. Wright-Doherty and trace element modelling support fractional crystallization of 14.1% plagioclase (An88), 6.7% olivine (Fo86), and 4.7% clinopyroxene (Wo41En49Fs10) from 483-17-2-(78-83) to form the least differentiated sample with Mg# = 63. The La/Sm_cn of this derivative magma is almost identical to the parent magma (0.35 to 0.36), but the other samples have higher La/Sm_cn (0.45 to 0.51), more total REE, and lower Mg# (60 to 56). Both Wright-Doherty and trace element modelling indicate that the primary magma chosen cannot produce these more evolved samples. For the major elements, the TiO2 and P2O5 are too low in the calculated versus the observed (1.38 to 1.90; 0.11 to 0.17, respectively, for example). Rayleigh fractionation calculates a lower La/Sm_cn and requires about 60% crystal removal versus 40% for the Wright-Doherty. These more evolved samples must be derived from a parent magma different from the one selected here and, unfortunately, not sampled in this study. A magma formed by a smaller degree of partial melting with slightly more residual clinopyroxene left in the mantle than for sample 483-17-2-(78-83) is required.

Images of a groundwater flow system in Nicaragua

Conceptualization of groundwater flow systems is necessary for water resources planning. Geophysical, hydrochemical and isotopic characterization methods were used to investigate the groundwater flow system of a multi-layer fractured sedimentary aquifer along the coastline in Southwestern Nicaragua. A geologic survey was performed along the 46 km2 catchment. Electrical resistivity tomography (ERT) was applied along a 4.4 km transect parallel to the main river channel to identify fractures and determine aquifer geometry. Additionally, three cross sections in the lower catchment and two in hillslopes of the upper part of the catchment were surveyed using ERT. Stable water isotopes, chloride and silica were analyzed for springs, river, wells and piezometers samples during the dry and wet season of 2012. Indication of moisture recycling was found although the identification of the source areas needs further investigation. The upper-middle catchment area is formed by fractured shale/limestone on top of compact sandstone. The lower catchment area is comprised of an alluvial unit of about 15 m thickness overlaying a fractured shale unit. Two major groundwater flow systems were identified: one deep in the shale unit, recharged in the upper-middle catchment area; and one shallow, flowing in the alluvium unit and recharged locally in the lower catchment area. Recharged precipitation displaces older groundwater along the catchment, in a piston flow mechanism. Geophysical methods in combination with hydrochemical and isotopic tracers provide information over different scales and resolutions, which allow an integrated analysis of groundwater flow systems. This approach provides integrated surface and subsurface information where remoteness, accessibility, and costs prohibit installation of groundwater monitoring networks.

Geochemistry and ages at DSDP Hole 19-192A

Conventional K-Ar and 40Ar/39Ar age data on altered basalts from DSDP Hole 192A on Meiji Guyot, Emperor Seamount chain, indicate a minimum age for the volcano of 61.9 ± 5.0 m.y. The K-Ar data are consistent with the early Maestrichtian date of the overlying sediments, but do not provide either a positive or negative test of the hypothesis that Meiji is older than Emperor volcanoes to the south. The most prominent alteration affecting the age measurements is potassium metasomatism, particularly of feldspar phenocrysts. The K-Ar apparent ages of feldspar separates from the Meiji basalts show that more than half of the potassium metasomatism occurred within the last 25 m.y. or so, and that if the potassium replacement rate has been constant, then the alteration of the Meiji basalts did not begin for 10 to 20 m.y. after the volcano formed.