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Hydrogeology EEES 4410/5410 Jamie M. Martin-Hayden Associate Professor (419) 530-2634 [email protected] Hydrogeology Defined Water Earth Earth materials • • • Rock Sediment (Soil) Fluids (Water) Geologic processes • • • Form, Transform and Distribute (redistribute) Earth materials Water is a primary agent of many (all?) geologic processes Hydrogeology Defined Water Earth Interactions Interactions go both ways Groundwater controls geologic processes. Geology controls flow and availability of groundwater. Hydrogeology Defined Water Earth Interactions Geology controls groundwater flow Permeable pathways are controlled by distributions of geological materials. E.g., Artesian (confined) aquifer Hydrogeology Defined Water Earth Interactions Geology controls groundwater flow Permeable pathways are controlled by distributions of geological materials. Groundwater availability is controlled by geology. Hydrogeology Defined Water Earth Interactions Geology controls groundwater flow Permeable pathways are controlled by distributions of geological materials. Groundwater availability is controlled by geology. Subsurface contaminant transport in is controlled by geology. Hydrogeology Defined Water Earth Interactions Groundwater controls geologic processes Igneous Rocks: Groundwater controls water content of magmas. Metamorphic Rocks: Metasomatism (change in composition) is controlled by superheated pore fluids. Volcanism: Geysers are an example of volcanic activity interacting with groundwater. Hydrogeology Defined Water Earth Interactions Groundwater controls geologic processes Landforms: Valley development and karst topography are examples of groundwater geomorphology. Landslides: Groundwater controls slope failure. Earthquakes: Fluids control fracturing, fault movement, lubrication and pressures. Hydrogeology Subdisciplines Water resource evaluation What controls how much groundwater is stored and can be safely extracted? What controls where groundwater comes from and where it flows? What controls natural water quality: natural interactions with geological materials control the chemistry of groundwater? How can we protect groundwater recharge areas and groundwater reservoirs from contamination and depletion? Hydrogeology Subdisciplines Contaminant Hydrogeology Anthropogenic effects: degradation of water quality due to human influences (contamination) How fast are dissolved contaminants carried by groundwater? Transport pathways of contaminants: Where are sources of contamination impacting the groundwater, where are the going and what are the destinations? Remediation (clean-up) of contaminants dissolved in the groundwater. Ohio Groundwater Law 1843: Acton v. Blundell “English Rule” The landowner can pump groundwater at any rate even if an adjoining property owner were harmed. 1861: Frazier v. Brown English Rule in Ohio Groundwater is “…occult and concealed…” and legislation of its use is “…practically impossible.” Wisconsin Groundwater Law 1903: Huber v. Merkel English Rule in Wisconsin 1974: Wisconsin v. Michels Pipeline Constructors Inc. English Rule Overturned A property owner can pump unlimited amounts of groundwater, even with malicious harm Landowners no longer have “an absolute right to use with to a neighbor. impunity all water that can be pumped from the subsoil underneath.” English Rule Overturned in Ohio 1984: Cline v. American Aggregates English Rule overturned in Ohio Justice Holmes: “Scientific knowledge in the field of hydrology has advanced in the past Today: Lingering effects decade…” so it of English Rule “…can establish the cause and It is very difficult to prove effect relationship of the tapping of cause and effect to be underground water to the existing defensible in court. water level.”