{"id":59074,"date":"2024-04-30T07:18:44","date_gmt":"2024-04-30T07:18:44","guid":{"rendered":"https:\/\/ingeoexpert.com\/en\/?post_type=product&#038;p=59074"},"modified":"2026-06-15T07:21:09","modified_gmt":"2026-06-15T07:21:09","slug":"an-overview-of-quantitative-hydrogeology-including-groundwater-modeling-with-modflow","status":"publish","type":"product","link":"https:\/\/ingeoexpert.com\/en\/courses-online\/an-overview-of-quantitative-hydrogeology-including-groundwater-modeling-with-modflow\/","title":{"rendered":"Introduction to Quantitative Hydrogeology and Groundwater Modeling with MODFLOW"},"content":{"rendered":"<h3 style=\"text-align: left;\">Introduction<\/h3>\n<p>Quantitative hydrogeology entails the development and application of quantitative tools and approaches for understanding the flow of water through soil and aquifer systems in the near-surface environment. This includes a vast array of subtopics, ranging from estimating rates of groundwater flow from potentiometric surface measurements and hydraulic conductivity distributions, interpretation of pumping tests, understanding the unsaturated flow of water through the vadose zone in response to different boundary conditions, and predicting the flow patterns of groundwater in heterogeneous aquifers using mathematical tools ranging from simple analytical models to sophisticated numerical simulators. In a future likely to be characterized by water scarcity and climate change impacts, an understanding of how to characterize and model these types of problems \u2013 and many more \u2013 will be essential for protecting and optimizing the use of groundwater resources.<\/p>\n<h3 style=\"text-align: left;\" align=\"left\">Objectives<\/h3>\n<p>This course will provide an introduction to a variety of concepts in quantitative hydrogeology, with a strong focus on applying the U.S. Geological Survey\u2019s MODFLOW groundwater flow model and its various supporting packages to demonstration examples. These examples will vary in complexity and will encompass a range of processes occurring across different spatial scales. In addition to MODFLOW, other quantitative tools will be introduced and explored, including analytical flow models, approaches for modeling unsaturated flow through the vadose zone, and tracing groundwater flow paths across potentiometric surfaces using scripting. All simulation tools used in the course will be available in the public domain for download or else custom-developed for the course; no commercial software license purchases will be required.<\/p>\n<p>At the conclusion of the course, students will:<\/p>\n<ul>\n<li>Understand key quantitative hydrogeologic concepts and parameterizations, including Darcy\u2019s law and the continuity equation, hydraulic conductivity, aquifer storage, saturation-dependent unsaturated flow through the vadose zone, and techniques for modeling recharge, evapotranspiration, and dynamically linking groundwater flow with surface water bodies (streams and lakes)<\/li>\n<li>Be able to construct MODFLOW models for a variety of aquifer environments across different spatial scales. Specifically, the course will rely upon MODFLOW-6 and the U.S. Geological Survey\u2019s ModelMuse graphical user interface.<\/li>\n<li>Understand how to use spreadsheets and scripting to analyze groundwater flow problems.<\/li>\n<\/ul>\n<p>The course will be presented through the use of multimedia explanatory exercises, instructional videos, and webinars that involve working through specific example applications.<\/p>\n<p>Please note that while the course will provide a brief introduction to the topic of solute transport in groundwater, this will not be a principal focus area.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Introduction Quantitative hydrogeology entails the development and application of quantitative tools and approaches for understanding the flow of water through soil and aquifer systems in the near-surface environment. This includes a vast array of subtopics, ranging from estimating rates of groundwater flow from potentiometric surface measurements and hydraulic conductivity distributions, interpretation of pumping tests, understanding [&hellip;]<\/p>\n","protected":false},"featured_media":59077,"comment_status":"open","ping_status":"closed","template":"","meta":{"_acf_changed":false,"_uf_show_specific_survey":0,"_uf_disable_surveys":false,"ocean_post_layout":"","ocean_both_sidebars_style":"","ocean_both_sidebars_content_width":0,"ocean_both_sidebars_sidebars_width":0,"ocean_sidebar":"0","ocean_second_sidebar":"0","ocean_disable_margins":"enable","ocean_add_body_class":"","ocean_shortcode_before_top_bar":"","ocean_shortcode_after_top_bar":"","ocean_shortcode_before_header":"","ocean_shortcode_after_header":"","ocean_has_shortcode":"","ocean_shortcode_after_title":"","ocean_shortcode_before_footer_widgets":"","ocean_shortcode_after_footer_widgets":"","ocean_shortcode_before_footer_bottom":"","ocean_shortcode_after_footer_bottom":"","ocean_display_top_bar":"default","ocean_display_header":"default","ocean_header_style":"","ocean_center_header_left_menu":"0","ocean_custom_header_template":"0","ocean_custom_logo":0,"ocean_custom_retina_logo":0,"ocean_custom_logo_max_width":0,"ocean_custom_logo_tablet_max_width":0,"ocean_custom_logo_mobile_max_width":0,"ocean_custom_logo_max_height":0,"ocean_custom_logo_tablet_max_height":0,"ocean_custom_logo_mobile_max_height":0,"ocean_header_custom_menu":"0","ocean_menu_typo_font_family":"0","ocean_menu_typo_font_subset":"","ocean_menu_typo_font_size":0,"ocean_menu_typo_font_size_tablet":0,"ocean_menu_typo_font_size_mobile":0,"ocean_menu_typo_font_size_unit":"px","ocean_menu_typo_font_weight":"","ocean_menu_typo_font_weight_tablet":"","ocean_menu_typo_font_weight_mobile":"","ocean_menu_typo_transform":"","ocean_menu_typo_transform_tablet":"","ocean_menu_typo_transform_mobile":"","ocean_menu_typo_line_height":0,"ocean_menu_typo_line_height_tablet":0,"ocean_menu_typo_line_height_mobile":0,"ocean_menu_typo_line_height_unit":"","ocean_menu_typo_spacing":0,"ocean_menu_typo_spacing_tablet":0,"ocean_menu_typo_spacing_mobile":0,"ocean_menu_typo_spacing_unit":"","ocean_menu_link_color":"","ocean_menu_link_color_hover":"","ocean_menu_link_color_active":"","ocean_menu_link_background":"","ocean_menu_link_hover_background":"","ocean_menu_link_active_background":"","ocean_menu_social_links_bg":"","ocean_menu_social_hover_links_bg":"","ocean_menu_social_links_color":"","ocean_menu_social_hover_links_color":"","ocean_disable_title":"default","ocean_disable_heading":"default","ocean_post_title":"","ocean_post_subheading":"","ocean_post_title_style":"","ocean_post_title_background_color":"","ocean_post_title_background":0,"ocean_post_title_bg_image_position":"","ocean_post_title_bg_image_attachment":"","ocean_post_title_bg_image_repeat":"","ocean_post_title_bg_image_size":"","ocean_post_title_height":0,"ocean_post_title_bg_overlay":0.5,"ocean_post_title_bg_overlay_color":"","ocean_disable_breadcrumbs":"default","ocean_breadcrumbs_color":"","ocean_breadcrumbs_separator_color":"","ocean_breadcrumbs_links_color":"","ocean_breadcrumbs_links_hover_color":"","ocean_display_footer_widgets":"default","ocean_display_footer_bottom":"default","ocean_custom_footer_template":"0"},"product_brand":[],"product_cat":[499,500,497,498,501,503],"product_tag":[],"class_list":["post-59074","product","type-product","status-publish","has-post-thumbnail","product_cat-civil-engineering","product_cat-environmental-science","product_cat-geology","product_cat-geotechnical-engineering","product_cat-mining","product_cat-software","entry","has-media","first","instock","sold-individually","shipping-taxable","purchasable","product-type-variable","has-rating","has-product-nav","col","span_1_of_3","owp-content-center","owp-thumbs-layout-horizontal","owp-btn-normal","owp-tabs-layout-horizontal","has-no-thumbnails"],"acf":[],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v27.6 - 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