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This video is about the storativity (S) of aquifers, also known as the storage coefficient. Storativity is a key parameter which we need for groundwater resources studies. We will look at the key concepts of storativity in unconfined aquifers - specific yield (Sy) & specific retention (Sr), and confined aquifers - specific storage (Ss) & storativity (S). In confined aquifers we will discuss the concepts of aquifer compressibility (total stress, effective stress & pore fluid stress) and water compressibility. We will do an example calculation of storativity for a sandy gravel aquifer using published alpha & beta values. 00:00 Introduction 01:13 Definition of storativity 01:38 Specific yield in an unconfined aquifer 03:25 Storativity in a confined aquifer 05:19 Definition of specific storage 06:19 Definition of storativity 07:07 Typical ranges of storativity in confined aquifers 07:59 Sources of water when confined aquifers are decompressed 08:17 Mechanism 1: Compression of the aquifer 11:54 Definition of compressibility (alpha) 12:26 Mechanism 2: Expansion of water 12:54 Definition of water compressibility (beta) 13:10 Equations for specific storage (Ss) and storativity (S) 15:45 Summary and conclusions Link to Excel Storativity Calculator: https://bit.ly/3wkPFlx This is an educational video & part of the Hydrogeology 101 course. #Hydrogeology #Storativity #StorageCoefficient