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The process of infiltration is not so simple. Below are some characteristics of infiltration and how they may affect the performance of a practice. Understanding these processes helps explain why stormwater practices may not perform as expected (either over- or under-perform). | The process of infiltration is not so simple. Below are some characteristics of infiltration and how they may affect the performance of a practice. Understanding these processes helps explain why stormwater practices may not perform as expected (either over- or under-perform). | ||
− | *'''Steady-state vs. transient flow'''. When we size a practice we either measure the steady-state infiltration rate using devices such as a <span title="The permeameter is a laboratory tool to measure the saturated permeability, or K-factor, of soil samples."> '''permeameter'''</span> or double-ring infiltrometer, or we take soil borings to determine the soil texture and then assign an infiltration rate (see [[Design infiltration rates]]), which is typically the saturated <span title="Hydraulic conductivity is a property of soils and rocks that describes the ease with which a fluid (usually water) can move through pore spaces or fractures."> '''hydraulic conductivity (k)'''</span> for that soil texture. But soils are rarely saturated at the beginning of a rainfall/runoff event. Consequently some infiltration occurs prior to development of a <span title="The interface between soil that is unchanged from the initial state and the newly wetted zone from an infiltration or irrigation event."> '''wetting front'''</span> in a soil. The adjacent schematic indicates infiltration rates | + | *'''Steady-state vs. transient flow'''. When we size a practice we either measure the steady-state infiltration rate using devices such as a <span title="The permeameter is a laboratory tool to measure the saturated permeability, or K-factor, of soil samples."> '''permeameter'''</span> or double-ring infiltrometer, or we take soil borings to determine the soil texture and then assign an infiltration rate (see [[Design infiltration rates]]), which is typically the saturated <span title="Hydraulic conductivity is a property of soils and rocks that describes the ease with which a fluid (usually water) can move through pore spaces or fractures."> '''hydraulic conductivity (k)'''</span> for that soil texture. But soils are rarely saturated at the beginning of a rainfall/runoff event. Consequently some infiltration occurs prior to development of a <span title="The interface between soil that is unchanged from the initial state and the newly wetted zone from an infiltration or irrigation event."> '''wetting front'''</span> in a soil. The adjacent schematic indicates how infiltration rates vary with soil water (moisture) content. For more information on soil infiltration, see these sites. |
**[[Soil hydrologic properties and processes]] | **[[Soil hydrologic properties and processes]] | ||
**[[Determining soil infiltration rates]] | **[[Determining soil infiltration rates]] | ||
+ | **[https://www.mdpi.com/2076-3417/12/12/6185 Wetting Front Expansion Model for Non-Ponding Rainfall Infiltration in Soils with Uniform and Non-Uniform Initial Moisture Content] - Yao et. al, 2022. Appl. Sci. 12(12):6185. https://doi.org/10.3390/app12126185 | ||
*'''One-dimensional flow'''. In designing an infiltration practice we assume all water is transported vertically. Infiltration of course occurs in three dimensions. This increases the area over which infiltration is occurring. Thus, using the surface area of a practice to size a practice underestimates the actual area over which infiltration is occurring. Wetting fronts in sandy soils are more elongated compared to loams and clays. For more information, watch these videos and see the adjacent image. | *'''One-dimensional flow'''. In designing an infiltration practice we assume all water is transported vertically. Infiltration of course occurs in three dimensions. This increases the area over which infiltration is occurring. Thus, using the surface area of a practice to size a practice underestimates the actual area over which infiltration is occurring. Wetting fronts in sandy soils are more elongated compared to loams and clays. For more information, watch these videos and see the adjacent image. | ||
**[https://www.youtube.com/watch?v=ptBlPBK_Zxs The wetting front] | **[https://www.youtube.com/watch?v=ptBlPBK_Zxs The wetting front] | ||
**[https://www.youtube.com/watch?v=gYk07ZGZbqo Detecting the wetting front] | **[https://www.youtube.com/watch?v=gYk07ZGZbqo Detecting the wetting front] | ||
*'''Homogenous soils'''. We strongly recommend measuring infiltration rate in the field and taking multiple measurements. The reason is that soils are not homogenous. Ksat varies considerably over relatively short distances, even within an area having a single mapped soil unit. It is not uncommon for Ksat to vary by up to three orders of magnitude at a single development site ([https://www.sciencedirect.com/science/article/abs/pii/S0169555X1930251X], [https://www.researchgate.net/publication/256706850_Variability_of_hydraulic_conductivity_due_to_multiple_factors], [https://agupubs.onlinelibrary.wiley.com/doi/abs/10.1029/WR012i001p00078], [https://www.publish.csiro.au/sr/sr99091], [https://acsess.onlinelibrary.wiley.com/doi/abs/10.2136/sssaj1971.03615995003500050058x]). [https://www.researchgate.net/publication/256706850_Variability_of_hydraulic_conductivity_due_to_multiple_factors Deb and Schukla] (2012, free access) provide a nice discussion of saturated hydraulic conductivity. | *'''Homogenous soils'''. We strongly recommend measuring infiltration rate in the field and taking multiple measurements. The reason is that soils are not homogenous. Ksat varies considerably over relatively short distances, even within an area having a single mapped soil unit. It is not uncommon for Ksat to vary by up to three orders of magnitude at a single development site ([https://www.sciencedirect.com/science/article/abs/pii/S0169555X1930251X], [https://www.researchgate.net/publication/256706850_Variability_of_hydraulic_conductivity_due_to_multiple_factors], [https://agupubs.onlinelibrary.wiley.com/doi/abs/10.1029/WR012i001p00078], [https://www.publish.csiro.au/sr/sr99091], [https://acsess.onlinelibrary.wiley.com/doi/abs/10.2136/sssaj1971.03615995003500050058x]). [https://www.researchgate.net/publication/256706850_Variability_of_hydraulic_conductivity_due_to_multiple_factors Deb and Schukla] (2012, free access) provide a nice discussion of saturated hydraulic conductivity. | ||
− | *'''Preferential flow'''. Preferential flow, often called short-circuiting, is the rapid movement of water and associated solutes in large soil pores (e.g. pores greater than 75 microns in diameter). For stormwater applications, macropore flow occurs primarily under saturated conditions since the rate of water delivery to a soil typically exceeds the soil infiltration rate, resulting in ponding. Soil microrelief can lead to locally saturated areas within a soil, initiating macropore flow in those areas. In soils with significant macroporosity, a high percentage of annual water and solute movement can occur within the macropores. Mechanisms of macropore development in infiltration bmps are not yet understood. For more information and links to references, [https://stormwater.pca.state.mn.us/index.php?title=Soil_hydrologic_properties_and_processes#Preferential_.28macropore.29_pore_flow_in_soil go here]. | + | *'''Preferential flow'''. Preferential flow, often called short-circuiting, is the rapid movement of water and associated solutes in soil. It is typically associated with transport in large soil pores (e.g. pores greater than 75 microns in diameter). For stormwater applications, macropore flow occurs primarily under saturated conditions since the rate of water delivery to a soil typically exceeds the soil infiltration rate, resulting in ponding. Soil microrelief can lead to locally saturated areas within a soil, initiating macropore flow in those areas. In soils with significant macroporosity, a high percentage of annual water and solute movement can occur within the macropores. Mechanisms of macropore development in infiltration bmps are not yet understood. For more information and links to references, [https://stormwater.pca.state.mn.us/index.php?title=Soil_hydrologic_properties_and_processes#Preferential_.28macropore.29_pore_flow_in_soil go here]. |
+ | :Preferential flow may also be associated with "fingering" in soil, which is the movement of water and solutes in high velocity zones of the soil. These zones are not specifically associated with macropores but instead result from variable characteristics in soil, such as non-uniform texture and areas of water-repellency. For a description of fingering in a sand, see [https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/97WR02407 Ritsema and Dekker, 1998]. | ||
*'''Time'''. Soil hydraulic properties change with time. There are two competing forces at work in an infiltration practice. First, water ponded in a practice exerts pressure on the underlying soil, resulting in some compaction at the soil surface. Counteracting this is the biologic activity in soil, including the impact of plant root growth, actions of soil invertebrates, and development of macropores in some practices. Unfortunately, there are few long-term studies of infiltration rates in stormwater infiltration bmps. Limited studies of systems, such as those conducted over a 5 year period, indicate hydrologic performance in infiltration practices is maintained if the practice was properly designed, constructed, and maintained. Similarly, more work is needed to understand seasonal changes in infiltration, which have been observed in studies conducted at Villanova University. | *'''Time'''. Soil hydraulic properties change with time. There are two competing forces at work in an infiltration practice. First, water ponded in a practice exerts pressure on the underlying soil, resulting in some compaction at the soil surface. Counteracting this is the biologic activity in soil, including the impact of plant root growth, actions of soil invertebrates, and development of macropores in some practices. Unfortunately, there are few long-term studies of infiltration rates in stormwater infiltration bmps. Limited studies of systems, such as those conducted over a 5 year period, indicate hydrologic performance in infiltration practices is maintained if the practice was properly designed, constructed, and maintained. Similarly, more work is needed to understand seasonal changes in infiltration, which have been observed in studies conducted at Villanova University. | ||
Over the past several years we've heard from people suggesting they be notified when updates are made to the Minnesota Stormwater Manual. We have also identified several stormwater management concerns and felt that focused communication on these specific issues might be useful. We therefore decided that periodic emails to subscribers would be one way of notifying practitioners about updates to the Manual and focus on specific stormwater issues. Emails are sent periodically, roughly every 6-12 weeks.
The emails contain only a short description of updates and other information. This page provides more detailed information. It is organized by the approximate dates when emails are sent to subscribers. We welcome recommendations for featured topics and links to case studies and other items of information. Please contact Mike Trojan at the MPCA..
Subscribe to the email list here.
We never got around to emailing an update in July, 2022, as we had planned. You can see what we did write in July, 2022 here.
Since our last email was 9 months ago, we have a lot of updates, so we'll try to be brief here and instead direct you to websites where you can get more information.
Here is a summary of recent updates to the wiki.
Apologies for the long article, but hopefully you'll find it informative and useful.
In the Minnesota Stormwater Manual we have dedicated a considerable amount of time and resources to the topic of infiltration. At the end of this article are some of the many pages containing information on this topic. Considering the energy expended on this topic, we've perhaps not spent enough time drilling into the process of water infiltration into soil. So put on your physics cap.
In the context of stormwater, infiltration is simply the movement of water through soil or engineered media within a stormwater practice ( best management practice) and into the underlying soil, vadose zone, and potentially groundwater. Infiltration occurs in nearly all stormwater practices, even those employing liners, since liners are not impermeable - they just have very slow infiltration rates. But even in filtration practices such as bioretention with an underdrain ( biofiltration), annual losses of water to infiltration commonly exceed 5 percent and often reach into the teens of percentages (determined from MIDS Calculator modeling).
Here we are concerned only with practices designed to infiltrate stormwater runoff. For a discussion of these practices, see Stormwater infiltration Best Management Practices and BMPs for stormwater infiltration. These practices are the focus of this discussion because they are designed (sized) to capture and infiltrate a specified amount of stormwater runoff, typically called a performance goal. Example performance goals are the 1 inch requirement in the Construction Stormwater General Permit and the 1.1 inch goal for Minimal Impact Design Standards. In sizing these practices, we typically configure the practice surface area and depth to instantaneously capture the performance goal ( instantaneous volume), often called the kerplunk method or estimation. For example, to meet a 1 inch performance goal from one acre of impervious surface, we "kerplunk" 3630 cubic feet of water into the practice, then sit back and expect it to infiltrate within 48 hours (or 24 hours in some cases). We base this expectation on the properties of the soil into which the water infiltrates.
The process of infiltration is not so simple. Below are some characteristics of infiltration and how they may affect the performance of a practice. Understanding these processes helps explain why stormwater practices may not perform as expected (either over- or under-perform).
So what does all this mean when designing an infiltration system? Some possible take-home messages include the following.
To better understand some of these principles in stormwater applications, we recommened A new dynamic horizon in stormwater, presented by Dr. Bridget Wadzuk at the Minnesota Seminar and Spotlight Series.
Suggested pages in the Minnesota Stormwater Manual
Although it has been several months since the last update to the Stormwater Manual wiki, we have not added a lot of new material. However, we are beginning a review and reorganization process for the wiki.
We are continually bombarded with new terminology and acronyms. These days, an important focus of stormwater is green infrastructure, anture-based solutions, and sustainability. What do these mean and is it important to know the distinction between these?
To begin, there is no universal definition of these. So this featured article provides our view on this topic. If you want some basic definitions, we have a page called Green infrastructure and green stormwater infrastructure terminology.
The core concept is that we receive all our resources, needs, and provisions from nature. Examples include clean air and water, nutrient cycling, pollination, and minerals. These may become depleted or impaired as we utilize these ecosystem services, making them unavailable for future generations. This is not sustainable, since at some point lack of one or more ecosystem services will make life untenable. To become sustainable, we must utilize ecosystem services in a way that keeps them useable into the future.
One way to achieve sustainable development is to design and build systems that mimic nature. This is done by conserving resources or engineering systems that retain or simulate natural processes. These systems include transportation, buildings, utilities, air and water management, waste management, and so on. Concepts incorporating these different features typically occur at the watershed, city, or large development scale and include the following.
Stormwater is one factor to consider in sustainable development.
It's been several months since our last update, as we were wrapping up a number of projects.
It is widely acknowledged the most effective strategy for protecting receiving waters from chloride pollution is by reducing use of chloride-deicers. But elimination of deicers is not practical in the foreseeable future. Are there ways to manage urban runoff having elevated chloride concentrations?
A workgroup of stormwater and groundwater professionals recently produced a white paper, published by the Minnesota Groundwater Association, that addresses this topic. The paper, titled Impacts of Stormwater Infiltration on Chloride in Minnesota Groundwater, provides a discussion of chloride in stormwater runoff and potential groundwater impacts associated with infiltration of stormwater runoff.
Chloride concentrations in stormwater runoff are highly variable and seasonally dependent. Concentrations in winter range from several hundred mg/L to as high as 40,000 mg/L, with typical concentrations being closer to 1000 mg/L. Concentrations outside the deicing season are typically less than 50 mg/L, with concentrations decreasing from spring into fall. Chloride is toxic to aquatic life, with the aquatic life standard being 230 mg/L. The drinking water standard is based on taste and is 250 mg/L. Chloride is also toxic to vegetation, can corrode materials, and can inhibit lake mixing, which may in turn result in changes in phosphorus cycling.
Though chloride is not retained in soil, studies indicate it is attenuated in soil. As a result, there is a lag time between chloride entering soil, including a media-based stormwater best management practice, and its eventual movement to a receiving water, be that a lake, stream, river, or aquifer. Understanding this process and the eventual receiving water can help us manage runoff containing chloride. The white paper provides the following conclusions.
The white paper also provides several recommendations for managing stormwater runoff that contains elevated concentrations of chloride.
When snowmelt runs off from a surface or snow storage area, routing the meltwater across a permeable surface allows some infiltration and may slow the rate of delivery to the conveyance system. This may spread the delivery of chloride-rich water to receiving waters and smooth the peaks in chloride concentration in the receiving water.
The MIDS Calculator and MPCA Simple Estimator
The Minimal Impacts Design Standards (MIDS) Calculator and MPCA's Simple Estimator (Estimator) are two tools used to estimate volume and pollutant load reductions associated with implementation of stormwater control measures, also known as best management practices (BMPs). Each of these tools is widely used. The MIDS Calculator, for example, has had over 8000 downloads in the past 3 years, while the Estimator is used by many MS4 permittees to assess progress toward or determine if they are meeting a TMDL Wasteload Allocation. The advantage of these tools is they are relatively easy to use and understand. However, with simplicity comes the potential for inaccuracy. This article provides a high level discussion of these two tools, including their advantages and potential pitfalls. The closing paragraph in this article provides a discussion of how MPCA hopes to move forward in providing a better understanding and application of these tools.
MIDS Calculator
The MIDS Calculator was originally designed as a tool for determining how to meet the MIDS performance goal of 1.1 inches at development sites. Detailed discussion of the Calculator and MIDS performance goal are found on the following pages.
Despite the original intent, the Calculator is being used for purposes other than assessing volume reduction at individual sites. It was and continues to be widely used for water quality determinations, including at sub-watershed scales. This presents a number of challenges since the Calculator is not easily modified or is inflexible in addressing water quality at these larger scales. Examples of some limitations of the Calculator include the following.
These are just examples of limitations.
Fundamentally, the MIDS Calculator is limited by its platform. It is built in Excel and addressing these various issues would be challenging. Additionally, as these issues get addressed, the tool becomes more complex to use, defeating one of its original intentions.
MPCA Simple Estimator
The 2013 MS4 permit required quantification of pollutant reductions to demonstrate a permittee was making progress toward achieving or had achieved a TMDL ( total maximum daily load) wasteload allocation. The tools available, such as P8, WinSLAMM, SWMM, and even the MIDS Calculator, were accessible only to "modeling experts". As a result, the MPCA developed a simple Excel spreadsheet that employed the Simple Method. This spreadsheet was readily accessible to most practitioners and could be used to demonstrate progress toward meeting a WLA.
The tool was intended to be used for demonstrating progress toward reducing pollutant loads, since it only considered a single watershed and there was limited guidance on modifying defaults in the spreadsheet. To make the tool more robust and rigorous, the Excel workbook was updated to include up to 10 subwatersheds (as separate worksheets), default values were updated based on literature reviews, and guidance for using the tool was expanded. The tool was again widely used by permittees during the 2020-21 permit cycle. Questions and submittals we received indicated the tool continues to have limitations and is not being correctly applied in some situations. Some of the limitations in the tool include the following.
Addressing these issues
MPCA hopes to conduct a more rigorous analysis of how these tools are being used and develop appropriate guidance. Additional training is likely. The Estimator may undergo modifications based on this analysis. Unfortunately, changes to the MIDS Calculator are unlikely as the Excel platform is limiting in terms of adjusting the Calculator for water quality modeling. We are in the process of documenting some of these issues and hope to have more detailed guidance and training in place in 2022.
Alternative models may be used. The Minnesota Stormwater Manual provides a detailed summary of available water quality models. These models typically require greater modeling expertise and lack extensive documentation in the Manual, though many have user guides. The MPCA will also accept other modeling approaches, but it is recommended that permittees consult the MPCA prior to using alternative models.
Take the green infrastructure O&M quiz
The Minnesota Construction Stormwater Permit requires pretreatment for filtration and infiltration practices. Forebays or other pretreatment practices are highly recommended for constructed stormwater ponds. The permit, however, does not specify the type of or sizing for pretreatment practices. We are discovering that many stormwater best management practices (bmps, also often called stormwater control measures or scms) are not performing as designed, often due to heavy sediment loads to the bmp and to poor design.
Proper pretreatment can extend the life and improve performance of downstream bmps. But we frequently hear stories about inadequate or improperly designed pretreatment. This is unfortunate, since the Manual contains a wealth of information on pretreatment. For example, did you know the Manual contains the following?
Below are examples of some design issues that have been brought to our attention.
The information in the manual could be better organized and made more accessible. So, we hope to execute a work order this summer to better organize the information on pretreatment. You can help by providing the following (NOTE: We cannot endorse or promote specific commercial products, processes, or services).