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HYDROLOGICAL AND GEOCHEMICAL TRENDS AND PATTERNS IN THE UPPER RIO GRANDE, 1975 TO 1999 1
Author(s) -
Passell Howard D.,
Dahm Clifford N.,
Bedrick Edward J.
Publication year - 2004
Publication title -
jawra journal of the american water resources association
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.957
H-Index - 105
eISSN - 1752-1688
pISSN - 1093-474X
DOI - 10.1111/j.1752-1688.2004.tb01014.x
Subject(s) - hydrology (agriculture) , geological survey , trend analysis , environmental science , water quality , total dissolved solids , linear regression , fluoride , mineralogy , geology , chemistry , environmental engineering , ecology , geotechnical engineering , machine learning , computer science , biology , paleontology , inorganic chemistry
Hydrological and geochemical spatial patterns and temporal trends were analyzed using U.S. Geological Survey (USGS) water quality data collected from 1975 to 1999 along the uppermost 600 km of the Rio Grande in Colorado and New Mexico. Data on discharge, specific conductivity (SC), total dissolved solids (TDS), pH, Ca 2+ , Na + , Mg 2+ , K + , HCO 3 − , SO 4 2‐ , Cl − , F − , and SiO 2 came from six USGS stations ranging from the Colorado‐New Mexico border to below Albuquerque, New Mexico. Linear regression, Kendall's S, and Seasonal Kendall's S’ were used to detect trends, and ANOVA was used to analyze spatial differences between stations. Statistically significant increasing trends occurred in SC, TDS, Ca 2+ , Na + , Mg 2+ , K + , Cl − , and F − in the uppermost reaches, and significant decreasing trends of SC, TDS, Ca 2+ , Mg 2+ , K + , HCO 3 − , and SO 4 2‐ occurred at the lower stations around Albuquerque. Both fluoride concentrations and pH values increased at and below Albuquerque over the study period. Discharge data show an increasing trend across all stations. Spatially, data for dissolved substances show generally linear upstream to downstream increases in concentrations in the upper four stations, with several notable nonlinear increases at and below Albuquerque (SC, TDS, Na + , Cl − ). Significant increases in pH appear at and below Albuquerque, relative to upstream stations, probably due to improved sewage treatment.