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The Piper diagram (Piper 1944) constitutes a useful tool in the interpretation of water chemistry.
Details regarding the geochemical interpretation of water samples can be found in Piper (1953) and Hem (1985).
This investigation constitutes a starting point for the interpretation of water adsorption hysteresis by means of scanning desorption measurements.
The interpretation of water analyses allowed the chemical characterization of rain and seepage water that were involved in the stone decay processes ongoing at Basílica da Estrela.
However, the interpretation of water diffusion data is complex and requires a priori information about anatomy and architecture of the pathway under investigation.
Activities combining these two technologies were designed to address ecosystem science learning goals for middle school students, and aid in their understanding and interpretation of water quality measurements.
In recent years, many studies have been done using PCA in the interpretation of water quality parameters (Gajbhiye et al 2010, 2015b), geomorphometric parameters (Sharma et al. 2009), etc.
These results are highly relevant for the design of monitoring schemes and for the correct interpretation of water quality data in terms of assessing the performance of environmental management measures.
Owing to ambiguities arising from the irregularity of the historical 3H input function since 1945, a unequivocal and straightforward interpretation of water transit times in Alpine tunnels is not possible.
And from this long-standing interpretation of water law came the current conflict in the Klamath.
In 1805, Joseph Louis Gay-Lussac and Alexander von Humboldt showed that water is formed of two volumes of hydrogen and one volume of oxygen; and by 1811 Amedeo Avogadro had arrived at the correct interpretation of water's composition, based on what is now called Avogadro's law and the assumption of diatomic elemental molecules.
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