2. Establishment of the School

The formal establishment of the New York State School of Industrial and Labor relations grew out of the thoughtful and vigorous action of a unique group of practical politicians who firmly believed, as they stated in their first report, that “Though we may legislate to the end of time, there will never be industrial peace and harmony without good faith, integrity, a high degree of responsibility, and a real desire to cooperate on the part of all parties concerned.

The ILR School at Fifty: Voices of the Faculty, Alumni & Friends (Full Text)

A collection of reflections on the first fifty years of the School of Industrial and Labor Relations at Cornell University. Compiled by Robert B. McKersie, J. Gormly Miller, Robert L. Aronson, and Robert R. Julian. Edited by Elaine Gruenfeld Goldberg. It was the hope of the compilers that the reflections contained in this book would both kindle memories of the school and stimulate interest on the part of future generations of ILRies who have not yet shared in its special history. Dedicated to the Memory of J. Gormly Miller, 1914-1995. Copyright 1996 by Cornell University. All rights reserved

Appendix A : Time Line, Events, Incidents, and Items of Note

Chronological listing of events, incidents and items of note, compiled by J. Gormly Miller, Boodie N. McGinnis (GR ’95), and Robert R. Julian.AppendixAtimelineILRat50.pdf: 1224 downloads, before Oct. 1, 2020

Cover, Dedication, Preface, Contents

The cover, dedication, preface, and content pages from The ILR School at Fifty, a collection of reflections on the first fifty years of the School of Industrial and Labor Relations at Cornell University. Compiled by Robert B. McKersie, J. Gormly Miller, Robert L. Aronson, and Robert R. Julian. Edited by Elaine Gruenfeld Goldberg.1st_section_of_ILRat50.pdf: 918 downloads, before Oct. 1, 2020

Relationship Of Geology, Physiography, Agricultural Land-Use, And Groundwater Quality In Southwest Georgia

Water samples were collected from 34 wells in the Claiborne aquifer in southwest Georgia. Land use/cover is principally forest, wetland, or agriculture. The aquifer is exposed surficially to the northwest but dips beneath confining beds to the southeast. The Claiborne aquifer is generally a fine‐ to medium‐grained quartz sand becoming more calcareous downdip and to the east. Well water was analyzed in the field for pH, electrical conductivity, alkalinity, hardness, and temperature, and in the laboratory for Cl, NH4, NO3, total N, total P, ortho‐P, SO4, K, Na, Ca, Mg, and Fe. Hardness gradually increases from 5 mg/1 updip to 162 mg/1 downdip and bicarbonate alkalinity follows the same trend reflecting variations in the aquifer lithology. Higher than normal nitrate concentrations (4‐6 mg/1) are found in ground water in the exposed updip portion of the aquifer in areas where agricultural land use for cropland is high. However, in forest‐covered areas, ground water in the exposed portion of the aquifer contains nitrate concentrations similar to the confined areas of the aquifer: less than 1 mg/1. Other chemical constituents measured do not show a discernible pattern of variation. One well near a fertilizer storage facility contains nitrate concentrations exceeding the Safe Drinking Water Standards, and other wells in the agricultural portion of the outcrop belt may seasonally exceed these limits