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Gravimetry: Overview01:05

Gravimetry: Overview

Gravimetric analysis is a quantitative method where the analyte is isolated and weighed directly or after conversion into a substance of known composition. Gravimetric analysis can be classified as precipitation, electrogravimetry, volatilization, and particulate gravimetry, based on the method used to isolate the analyte.
In precipitation gravimetry, the analyte is converted into a precipitate and weighed. For example, the silver content in a sample can be estimated by precipitating and...
Quality of Water01:19

Quality of Water

In concrete preparation, the quality of water is paramount as it affects the strength and durability of the concrete. Potable water is usually preferred; however, it must not have excessive sodium or potassium to prevent compromising the concrete's integrity. Water quality is typically evaluated based on impurities such as dissolved solids, chlorides, and sulfates, and its pH value is ideally between 6 and 8. Even slightly acidic natural water may be acceptable unless it contains harmful...
Testing Water Quality01:14

Testing Water Quality

When the quality of water for concrete preparation is uncertain, its impact on the setting time of cement and compressive strength of mortar is assessed by comparison with de-ionized or distilled water benchmarks. American Society for Testing and Materials (ASTM) C1602 requires the setting times to be within 90 minutes of the control, British Standard (BS) 3146:1980 allows a 30-minute variance in the initial setting, while British Standards European Norm (BS EN) 1008 specifies initial setting...
Precipitation and Co-precipitation01:17

Precipitation and Co-precipitation

Precipitation and coprecipitation methods can be used to separate a mixture of ions in a solution. In qualitative inorganic analysis, ions that form sparingly soluble precipitates with the same reagent are separated based on the differences in solubility products. For example, consider the separation of Cu(II) and Fe(II) ions by precipitation as insoluble sulfides. First, copper(II) sulfide is precipitated by the addition of acidic H2S, where the dissociation of H2S is suppressed. Adding H2S...

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Related Experiment Video

Updated: Jul 8, 2026

Soil Lysimeter Excavation for Coupled Hydrological, Geochemical, and Microbiological Investigations
10:30

Soil Lysimeter Excavation for Coupled Hydrological, Geochemical, and Microbiological Investigations

Published on: September 11, 2016

Tectonic influences on ground water quality: insight from complementary methods.

Sam Earman1, Brian J O L McPherson, Fred M Phillips

  • 1Division of Hydrologic Sciences, Desert Research Institute, Reno, NV 89512, USA. searman@dri.edu

Ground Water
|January 16, 2008
PubMed
Summary

Tectonic activity significantly influences groundwater systems. This study reveals unique hydrogeology in San Bernardino Valley due to its distinct geology, offering insights for tectonically active regions globally.

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Area of Science:

  • Hydrogeology
  • Tectonics
  • Geochemistry

Background:

  • Groundwater is vital for domestic use, agriculture, and biodiversity in the San Bernardino Valley.
  • Understanding groundwater systems is crucial for sustainable resource management in tectonically active areas.

Purpose of the Study:

  • To investigate the tectonic influences on groundwater systems in the San Bernardino Valley.
  • To compare the hydrogeology of the San Bernardino Valley with its neighboring basins.

Main Methods:

  • Major ion geochemistry
  • Isotope hydrology
  • Dissolved gas analysis
  • Aquifer testing
  • Geophysics
  • Geological examination

Main Results:

  • The San Bernardino Valley's hydrogeology differs significantly from adjacent basins in water quality, chemical evolution, storage, and residence time.
  • These differences are attributed to the unique geology, including a magmatically active accommodation zone.
  • A comprehensive understanding was achieved by integrating multiple investigation methods.

Conclusions:

  • The distinct geology of the San Bernardino Valley creates unique groundwater characteristics.
  • This basin can serve as a model for understanding groundwater chemical evolution in tectonically diverse regions worldwide.