1729 Mini-Blogs for EPASWMM5, AutoDesk Innovyze ICM SWMM, SWMM5+: SWMM 5 Aquifer has a Saturated and Unsaturated Zone

Wednesday, October 20, 2010

SWMM 5 Aquifer has a Saturated and Unsaturated Zone

Note: The unsaturated upper zone soil moisture varies between the initial upper zone moisture fraction to the porosity fraction for the soil. The soil moisture content is for the SWMM5 Aquifer which can cover more than one Subcatchment in your simulation network.

via Blogger http://www.swmm5.net/2013/07/swmm-5-aquifer-has-saturated-and.html

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SWMM456.COM (previously known as SWMM5.NET) is a mini-blog that provides short and concise articles about various topics related to Stormwater Management Model (SWMM). Each post on the blog is no more than 150-200 words (about 1300 characters) in length and aims to deliver instant information, opinion, or introduction on a specific topic related to SWMM. The blog covers a wide range of topics, including tips and tricks for using SWMM, case studies, software updates, and news related to the field of stormwater management. The goal of the blog is to provide useful and relevant information to SWMM users and professionals in the stormwater management industry in a quick and easy-to-digest format.

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You can see recent Posts in the Recent Post Section, Top Labels, Older Alphabetical Labels and Dated Archives. You can also search for Tags in the Google Search Box or the Custom Search Box. The above Tabs in the Menu are those sites and blogs that I think can help you. Pleasse send any further questions to robert.dickinson@gmail.com or robert.dickinson@innovyze.com if you have further questions or ideas. If you are a student and you want a general introduction to SWMM 5 please visit Wikipedia or the EPA Tab. Thanks for visiting!

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Wednesday, October 20, 2010

SWMM 5 Aquifer has a Saturated and Unsaturated Zone

SWMM 5 Aquifer has a Saturated and Unsaturated Zone

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Blog strategy to explain complex modeling concepts to non-modelers, while highlighting the beauty and majesty of domain knowledge: