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Water resources data, Massachusetts and Rhode Island, water year 1992
R.S. Socolow, T.S. Shepard, G.G. Girouard, R. A. Gadoury
1993, Water Data Report MA-RI-92-1
Water-resources data for the 1992 water year for Massachusetts and Rhode Island consists of stage, discharge, and water quality of streams; contents of lakes and reservoirs; and ground-water levels. This report contains discharge records for 77 gaging stations, month end contents for six lakes and reservoirs, water quality for nine...
Discharge-measurement system using an acoustic Doppler current profiler with applications to large rivers and estuaries
Michael R. Simpson, Richard N. Oltmann
1993, Water Supply Paper 2395
Discharge measurement of large rivers and estuaries is difficult, time consuming, and sometimes dangerous. Frequently, discharge measurements cannot be made in tide-affected rivers and estuaries using conventional discharge-measurement techniques because of dynamic discharge conditions. The acoustic Doppler discharge-measurement system (ADDMS) was developed by the U.S. Geological Survey using a vessel-mounted...
The Loma Prieta, California, Earthquake of October 17, 1989: Societal response
Dennis S. Coordinated by Mileti
1993, Professional Paper 1553
Professional Paper 1553 describes how people and organizations responded to the earthquake and how the earthquake impacted people and society. The investigations evaluate the tools available to the research community to measure the nature, extent, and causes of damage and losses. They describe human behavior during and immediately after the...
Summary of reported agriculture and irrigation water use in Lonoke County, Arkansas, 1991
T.W. Holland, C.A. Manning, K.L. Stafford
1993, Open-File Report 93-471
This report summarizes the 1991 water-use reporting through the Conservation District Office in Lonoke County, Arkansas. The number of withdrawal registrations for Lonoke County was 3,313 (2,587 groundwater and 726 surface water). Water with drawals reported during the registration process total 61.30 Mgal/d (59.50 Mgal/d groundwater and 1.80 Mgal/d surface...
Factors affecting areas contributing recharge to wells in shallow aquifers
Thomas E. Reilly, David W. Pollock
1993, Water Supply Paper 2412
The source of water to wells is ultimately the location where the water flowing to a well enters the boundary surface of the ground-water system. In ground-water systems that receive most of their water from areal recharge, the location of the water entering the ground-water system is at the water...