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Related Concept Videos

Precipitation Gravimetry01:03

Precipitation Gravimetry

Precipitation gravimetry is based on converting an analyte into a sparingly soluble precipitate, which is separated by filtration and weighed. An ideal precipitate should be pure, insoluble, of known composition, and easily filtered from the reaction mixture.
In determining nickel by gravimetric analysis, a precipitant of ethanolic dimethylglyoxime is added to a hot nickel salt solution. This is quickly followed by the dropwise addition of dilute ammonia solution until precipitation occurs. A...

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Updated: May 20, 2026

Methods of Soil Resampling to Monitor Changes in the Chemical Concentrations of Forest Soils
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Global Soil Water Stable Isotope Dataset.

Jiangwei Yang1,2,3, Rui Li1,2,3, Yitian Lei1

  • 1College of Geography and Environmental Science, Northwest Normal University, Lanzhou, 730070, Gansu, China.

Scientific Data
|April 18, 2026
PubMed
Summary
This summary is machine-generated.

A new global dataset of soil-water isotopes (2H and 18O) has been compiled, harmonizing fragmented historical data. This resource aids research into ecohydrology and global water cycling.

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Area of Science:

  • Earth and Environmental Sciences
  • Hydrology
  • Isotope Geochemistry

Background:

  • Soil water isotopes (2H and 18O) are crucial tracers for ecohydrological processes.
  • Existing soil-water isotope data are fragmented, lack standardization, and are unevenly distributed, hindering global research.

Purpose of the Study:

  • To compile and structurally harmonize a comprehensive global dataset of soil-water stable isotopes.
  • To address limitations in historical data for cross-regional and global-scale ecohydrological studies.

Main Methods:

  • Integrated primary in-situ measurements, literature records, and open-repository data.
  • Compiled 27,455 records from 463 sites across 37 countries (1975-2024).
  • Classified data into standardized soil profile intervals (shallow, active-root, mid-depth, deep) with metadata.

Main Results:

  • Created a globally representative dataset of soil-water stable isotopes.
  • The dataset spans 1975 to 2024, covering six continents.
  • Standardized data classification facilitates comparative analysis.

Conclusions:

  • The harmonized dataset provides a robust foundation for evaluating terrestrial water cycling.
  • Enables calibration of hydrological models and tracing of ecosystem water-use strategies.
  • Supports research on hydroclimatic challenges under global environmental change.