The present invention is directed at a passive infiltration drainage system configured to allow for drainage of excess water from grassy areas in urban and suburban settings. More particularly, the invention relates to an underground plurality of conveyance channels and a plurality of interconnected infiltration tunnels designed to drain surface water to desired and targeted storage areas.
The following description is not an admission that any of the information provided herein is prior art relevant to the present invention, or that any publication specifically or implicitly referenced is prior art. Any publications cited in this description are incorporated by reference herein. Where a definition or use of a term in an incorporated reference is inconsistent or contrary to the definition of that term provided herein, the definition of that term provided herein applies and the definition of that term in the reference does not apply.
In urban and suburban grassy areas like athletic fields and lawns, water pools tend to accumulate following heavy rainfall due to the stripping of organic matter and soil compaction. This prevents surface water from infiltrating, leading to pooling in low-lying areas without proper drainage.
Pooling water can damage grass, building foundations, and create mosquito breeding grounds. It also hinders recreational activities on fields and causes frustration for homeowners in personal yards.
Current drainage systems in urban and suburban areas are largely ineffective as they rely on water to permeate soil to reach drainage channels (e.g., U.S. Patent Application Publication 20210274729 A1). However, compacted soil often prevents water reaching these channels, as capillary forces draw water into fine pore spaces rather than draining into larger pore spaces.
Therefore, there exists a need for a method that can efficiently drain surface water from urban and suburban fields and yards without relying on soil permeation.
A passive infiltration drainage system is configured for transporting excess water from grassy areas in urban and suburban settings to desired storage areas that comprises a plurality of conveyance channels excavated in the landscape arranged in a network configuration; a plurality of infiltration tunnels excavated in the landscape that are connected to the plurality of conveyance channels configured for receiving and routing water flow; an optional water discharge outlet for collecting water from the plurality of conveyance channels; and bedrock or saprolite connected to the plurality of infiltration tunnels.
In one embodiment, the plurality of conveyance channels comprise sand.
In another embodiment, the plurality of conveyance channels is spaced about three to five feet apart, to a depth of about one to two feet, with a width of about one foot.
In still another embodiment, the plurality of conveyance channels is dug to a depth of about one to two feet.
In yet another embodiment, the plurality of conveyance channels is dug to a width of one foot.
In a further embodiment, the plurality of infiltration tunnels is drilled gradually upslope when adjacent to one or more structures that may be negatively impacted by excess water.
In one embodiment, the plurality of infiltration tunnels is drilled to a radius of 3 inches, and to a depth of 6 feet.
In yet another embodiment, the plurality of infiltration tunnels is drilled directly under impervious surfaces.
In an embodiment, the passive infiltration drainage system further comprises a sediment filter positioned in each of the plurality of conveyance channels, wherein the sediment filter comprises a sand top layer and clay base.
In an embodiment, the sand top layer is about 0.5 mm to 2 mm.
In yet another embodiment, the sand top layer comprises coarse sand and rounded sand.
In another embodiment, the clay is bentonite clay with a sediment size of 0.8 μm to 2000 μm.
In yet another embodiment, the bentonite clay is compacted to a thickness of 1 inch.
In a further embodiment, the conductive hydraulic substrate is saprolite.
In yet another embodiment, the passive infiltration drainage system further comprises an optional water discharge outlet directing collected water into a body of water adjacent to the drainage system.
In one embodiment, a passive infiltration drainage system comprises a plurality of conveyance channels; plurality of infiltration tunnels; bedrock or saprolite; and an optional water discharge outlet; wherein the system is configured to drain water from a land surface to the plurality of conveyance channels; the plurality of conveyance channels are configured to empty the water into the optional water discharge outlet; and the plurality of infiltration tunnels are configured to drain the water to a bedrock or saprolite.
In an embodiment, a method of draining water from a land surface to a desired storage area comprises the steps of draining the water from a land surface to a plurality of conveyance channels; and emptying the water from conveyance channels into an optional water discharge outlet.
In another embodiment, a method of draining water from a land surface to a desired storage area comprises the steps of draining the water from a land surface to a plurality of infiltration tunnels; and emptying the water from infiltration tunnels to a bedrock or saprolite.
The present disclosure is directed to a passive infiltration drainage system that drains water from the land surface to a desired storage area, comprising a plurality of conveyance channels, a plurality of infiltration tunnels, bedrock or saprolite, and an optional discharge outlet. The passive infiltration drainage system drains water from the land surface to a network of channels. The excess water is drained via the shallow channels to an optional water discharge outlet or into the bedrock or saprolite via the plurality of infiltration tunnels. The channels are dug 3 to 5 feet apart, to a depth of about 1 to 2 feet, with a width of about 1 foot. The cross-sectional area of the excavated channels is determined by the formula V=A*K (dz/dx), wherein V is the volumetric rate of flow, A is the cross-sectional area of the medium accommodating flow, K is the hydraulic conductivity of the medium, and dz/dx is the slope. The plurality of infiltration tunnels is then drilled to a radius of 3 inches, and to a depth of bedrock or a highly conductive hydraulic substrate. The optional water discharge outlet may be a body of water adjacent to the passive infiltration drainage system.
As used herein, and unless the context dictates otherwise, the term “system” is intended to mean passive infiltration drainage system. Therefore, the terms “system”, and “passive infiltration drainage system” are used synonymously.
As used in the description herein and throughout the claims that follow, the meaning of “a,” “an,” and “the” includes plural reference unless the context clearly dictates otherwise. Also, as used in the description herein, the meaning of “in” includes “into” and “on” unless the context clearly dictates otherwise.
As used herein, the term “about” in conjunction with a numeral refers to a range of that numeral starting from 10% below the absolute value of the numeral to 10% above the absolute value of the numeral, inclusive.
As used herein, and unless the context dictates otherwise, the term “channels” is intended to mean a plurality of excavated channels with a cross-sectional area calculated by the equation: V=A*K (dz/dx) wherein V is the volumetric rate of flow, A is the cross-sectional area of the medium accommodating flow, K is the hydraulic conductivity of the medium, and dz/dx is the slope. This equation, based on Darcy's Law, may be inverted to solve for the required cross-sectional area to accommodate the desired rate of volumetric flow.
As used herein, and unless the context dictates otherwise, the term “sand” is intended to mean a sediment size of about 0.5 mm to 2 mm.
As used herein, and unless the context dictates otherwise, the term “clay” is intended to mean compacted bentonite clay with a sediment size of about 0.8 μm to 2000 μm.
As used herein, and unless the context dictates otherwise, the term “tamper” is intended to mean a tool used to compress or pack material.
An exemplary configuration of water drainage through the passive infiltration drainage system 100 is schematically depicted in
An exemplary configuration for a conveyance channel system 200 is schematically depicted in
In another embodiment, the entire volume of the plurality of conveyance channels 101 is filled with coarse sand to create sand top layer 202. In another embodiment, water that flows to passive infiltration drainage system 100 as overland flow (i.e., surface runoff) is infiltrated directly into the plurality of conveyance channels 101 and conveyed laterally through sand top layer 202 at a rate of about 26.7 to 266.7 inches of water per day when placed at a slope of about 2 degrees. Water is preferentially conveyed laterally due to the hydraulic conductivity of the coarse sand exceeding that of the surrounding soils by 6 to 9 orders of magnitude (10{circumflex over ( )}6 to 10{circumflex over ( )}9), thus accommodating water along plurality of conveyance channels 101 even at a shallow slope (e.g., 0.01) at a rate that vastly exceeds the otherwise “natural” downward percolation of the water through the pre-existing substrate or bedrock at unit gradient (slope=1) by several orders of magnitude (10{circumflex over ( )}4 to 10{circumflex over ( )}7 times faster). In another embodiment, rounded sand sediments are selected for sand top layer 202 because this sediment class is resistant to soil compaction allowing water to flow through.
In another embodiment, each of plurality of conveyance channels 101 (comprising high hydraulic conductivity “coarse sand”) is dug within a layer of compacted urban soil 204. “Urban soils” are typically comprise clayey and loamy sediments that have been imported and highly compacted by construction equipment, reducing both the relative porosity (ability to hold water) and hydraulic conductivity (ability to convey water) by factors of 2-5 or 1,000 to 1,000,000,000, respectively. Non-compacted deep soils 205 (that are naturally more highly conductive than compacted “urban soils” by 3-9 orders of magnitude) are located below compacted urban soil 204. In this embodiment, non-compacted deep soil 205 continues downward until it reaches bedrock or saprolite 206 that is more hydraulically conductive by 3 to 9 orders of magnitude than the overlying soils, thus allowing the rapid lateral conveyance of excess water off property via the subsurface rather than the ponding of water on property on the less hydraulically conductive surface.
An exemplary configuration for plurality of infiltration tunnels 300 is schematically depicted in
Thus, specific embodiments for a passive infiltration drainage system and the method of using it have been disclosed. It should be apparent, however, to those skilled in the art that many more modifications besides those already described are possible without departing from the inventive concepts herein. The inventive subject matter, therefore, is not to be restricted except in the spirit of the appended claims. Moreover, in interpreting both the specification and the claims, all terms should be interpreted in the broadest possible manner consistent with the context. In particular, the terms “comprises” and “comprising” should be interpreted as referring to elements, components, or steps in a non-exclusive manner, indicating that the referenced elements, components, or steps may be present, or utilized, or combined with other elements, components, or steps that are not expressly referenced.
This application claims the benefit of U.S. Provisional Application No. 63/458,462, filed on Apr. 11, 2023, which is hereby incorporated in its entirety.
Number | Date | Country | |
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63458462 | Apr 2023 | US |