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<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:creator>Carole L. Thomas</dc:creator>
  <dc:date>1995</dc:date>
  <dc:description>Selected reaches of Grant Line Arroyo and Tijeras Arroyo in&#13;
Albuquerque, New Mexico, were studied to collect information &#13;
about the amount and quality of infiltration through arroyo &#13;
channels. Infiltration rate was calculated for selected reaches&#13;
of Grant Line Arroyo and Tijeras Arroyo based on instantaneous &#13;
streamflow-loss volumes, wetted channel area, and instantaneous &#13;
evaporation rates measured during 1988-92. Infiltration rates at&#13;
Grant Line Arroyo ranged from 0.0 to 0.6 foot per day, and at &#13;
Tijeras Arroyo from 2.28 to 30 feet per day. The evaporation&#13;
rate ranged from one-tenth of 1 percent to 2 percent of the &#13;
infiltration rate.&#13;
&#13;
     Infiltration rates differed with the location of the reach &#13;
isolated for measurement and with the time of day of the &#13;
infiltration-rate measurement. Differences in intrinsic &#13;
permeability of the sediments may be the most important factor &#13;
affecting spatial variations in infiltration. The most important&#13;
factor affecting temporal variations in infiltration may be the &#13;
temperature of the water and sediment where infiltration occurs.&#13;
&#13;
     Annual evaporation rates were greatest over saturated stream&#13;
sediments and ranged from 802 to 1,025 millimeters per year or &#13;
from 31.57 to 40.35 inches per year. Annual evaporation rates &#13;
were least over unsaturated, unvegetated soil and ranged from 174&#13;
to 291 millimeters per year or from 6.85 to 11.46 inches per&#13;
year. Annual evapotranspiration rates over grasses or shrubs or both &#13;
were about one-half the rates over saturated stream sediments.  &#13;
Rates were similar for Grant Line and Tijeras Arroyos. The land-&#13;
surface vegetation, availability of water at the land surface, &#13;
availability of energy to enable a change of state from water to&#13;
vapor, existence of a vapor concentration gradient, and a &#13;
turbulent atmosphere to carry the vapor away may be the factors &#13;
that determine the amount of evaporation and evapotranspiration.&#13;
&#13;
     Water in Grant Line Arroyo and Tijeras Arroyo met U. S. &#13;
Environmental Protection Agency drinking-water regulations for &#13;
nitrate, volatile organic compounds, dissolved lead, and &#13;
dissolved and total arsenic, barium, cadmium, chromium, copper, &#13;
iron, silver, zinc, selenium, chloride, and sulfate &#13;
concentrations. Total lead concentration in one sample from &#13;
Tramway Floodway Channel, a tributary to Tijeras Arroyo, was 55 &#13;
micrograms per liter, exceeding the Environmental Protection &#13;
Agency drinking-water regulation of 50 micrograms per liter.  &#13;
Dissolved-solids concentrations calculated from the sum of &#13;
cations and anions usually exceeded the Environmental &#13;
Protection Agency drinking-water dissolved-solids &#13;
regulation of 500 milligrams per liter at Tijeras Arroyo above &#13;
Four Hills Bridge.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/wri954070</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Infiltration and quality of water for two arroyo channels, Albuquerque, New Mexico, 1988-92</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>