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DRAINS

Drains are an important control method primarily used to drain water away from pyritic materials to limit the contribution of water in the formation of acidic drainage. Drains can be installed in various places at mine sites and rely on permeability contrasts between the drain and the permeability of waste rock, tailings, spoil, refuse and fills. There are several different types of drains including blanket drains, chimney drains, French drains, highwall drains and porous envelope. Selection of drain type depends on the purpose of the drain, location of the drain and estimated flow rates.
Drains are used to

  • Reduce the pore water pressures in the downstream portion of the dam therefore increasing the stability of the downstream slope against sliding.
  • Control any seepage that exits the downstream portion of the dam and prevent erosion of the downstream slope: i.e. to prevent 'piping'.

The effectiveness of the drain in reducing pore pressure depends on its location and extent. Piping can be controlled by making grading of the pervious material to meet the filter requirements for the embankment materials.
                                      
                                                    Figure 1, showing Piping,
                                  http://www.dur.ac.uk/~des0www4/cal/dams/emba/seep.htm

Blanket drains:
These are commonly used to drain water from surrounding soils or waste materials. The depth of these drains is normally three feet. The depth of these drains are increased significantly when need arises (i.e.), when the ground water table has to be lowered or to drain leachate. Cedergren (1989) states that to ensure that a blanket drain will be able to remove all the water that enters a structural section the minimum transmissibility’s can be estimated by Darcy’s law in the form of
kA = Q/i
Where Q is the quantity of water that needs to be removed by a drainage blanket,
‘i’ is the allowable hydraulic gradient,
k is the coefficient of permeability of the blanket and A is the cross sectional area normal to the direction of flow
The permeability must be sufficient to allow water to drain out before damage can occur. To prevent freezing in cold climates water that enters the system should drain in a relatively short time. Horizontal drainage blankets are often used for dams of moderate height. They are frequently used over the downstream one-half or one-third of the foundation area.
                             
                                                       Figure 2, Blanket Drain
                                  http://www.dur.ac.uk/~des0www4/cal/dams/emba/seep.htm

Disadvantages of blanket drains:
An earth dam embankment tends to be more pervious in the horizontal direction than in the vertical. Occasionally, horizontal layers tend to be much more impervious than the average material constructed into the embankment, so the water will flow horizontally on a relatively impervious layer and discharge on the downstream face despite the horizontal drain. Where this has occurred the downstream slope is prone to slipping and piping. Repairs can be made by installing pervious blankets on the downstream slopes or constructing vertical drains to connect with the horizontal blanket. Such vertical drains are normally composed of sand and gravel.
Toe drains: For low dams, a simple toe drain can be used successfully. Toe drains have been installed in some of the oldest homogeneous dams in an effort to prevent softening and erosion of the downstream toe.

                                  
                                                         Figure 3, Toe Drains,
                                http://www.dur.ac.uk/~des0www4/cal/dams/emba/seep.htm

Chimney drains:
Chimney drains have been used to avoid trouble due to stratification and to intercept water before it reaches downstream slope. Chimney drains collect water from a backfill or valley fill and convey water through a long, high column of coarse sand and drain runoff. Chimney drains are an attempt to prevent horizontal flow along relatively impervious stratified layers, and to intercept seepage water before it reaches the downstream slope. Chimney drains are often incorporated in high homogeneous dams, which have been constructed with inclined or vertical chimney drains.

For big dams, chimney drains have been inclined at a considerable slope, both upstream and sometimes downstream. An upstream inclined drain can act as a relatively thin core. In addition to controlling seepage through the dam and increasing the stability of the downstream slope, the chimney drain is also useful in reducing pore water pressures both during construction and following rapid reservoir drawdown.
                       
                                                                  Figure 4, Chimney drain,
                                             http://www.dur.ac.uk/~des0www4/cal/dams/emba/seep.htm

French Drains:
French drains collect sub-surface water from poorly drained areas and carry it to the main drainage line, dry well and ravine. It is constructed using materials like pea gravel or crushed rock, woven landscape fabric and perforated drainage pipe. Advantages of French drains are low cost, easy installation. After constructing they can be covered with a turf, making them less conspicuous.
Construction of a French Drain

  • A French drain starts with digging a trench. The depth and width of the trench can vary, but 5 to 6 inches wide and 8 to 12 inches deep are common sizes and usually satisfy most needs.
  • Grading is a critical consideration — you must ensure that enough slope exist for the water to actually flow, and flow in the right direction. It might be adequate to check very short stretches of drain with a level to ensure that a slope exists to carry water in the desired direction. However, you should take whatever measures are necessary, including a survey and grading, if needed, to ensure that you have at least a 0.5 percent slope. A 1 or 2 percent grade is better.
  • Add gravel to the trench to within a few inches of the surface. Gravel for this use is typically 0.5 to 1 inch in size.
  • On top of the gravel, lay at least 3 or 4 inches of coarse sand. This provides a medium in which turf can grow so that the trench will not be visible. But remember that the sand must be coarse or it won't allow water to properly drain through.

Turf may be seeded into the sand or simply allowed to grow in from the adjacent stand, if the turf is a spreading type. Or, you can lay sod over the sand. However, if you do this, be sure to wash the soil from the sod roots before laying it so that you don't contaminate the sand with finer soil.

                                              

                                     Figure 5, French Drain, http://www.createalandscape.com/Houston%20Drainage.htm

                                

                                   Figure 6, French Drain, http://handbooks.btcv.org.uk/handbooks/content/chapter/828

Highwall Drains:
Highwall drains collect ground water that enters a mine site before it comes in contact with mine spoils and distributes it through the site rapidly with minimal contact with the spoil. In this way the groundwater bypasses potentially acid-forming materials. Highwall drains can reduce the potential for acid mine drainage on sites with marginal overburden quality or can reduce the quantity of acid mine generation.
The design and installation of a highwall drain system must be customized to each site. Design parameters that must be considered include:

  • Where to place the drains
  • What materials to use
  • How to construct the drain system
  • The transport medium (i.e., pipe or rock)
  • Protection of the drain to ensure that it is not crushed during backfilling.

It is crucial that the drain systems are designed in a way that allows all groundwater to be collected where it enters a mine site; this may be at the highwall, endwall, or even the lowwall. It is equally important to ensure that drains are constructed in a matter that allows for positive drainage.

Drains can be constructed in three different methods:

The first drain construction technique initiates with the excavation of a small channel in the pit floor with a backhoe or similar equipment to a depth just sufficient (about 1 ft (0.3 m)) to capture groundwater from the highwall. A pipe (4 or 6 in (10-15 cm)) is then placed in the bottom of the channel and covered with gravel or coarse-grained material. Then, to prevent infiltration of sediment, which could plug the pipe, filter fabric is installed over the ditch.

The second method is to install a pipe at the low spot of each pit and allow water to naturally flow into it. This method does not include any disturbance of the underclay. In the one instance where this method was used, an inert 2 ft (0.6 m) compacted clay seal was placed on the pit floor under and on either side of the pipe; this permitted groundwater flow along the top of the inert clay rather than on the acidic underclays.

The third procedure is generally the same as the first but does not use pipes. Using this approach, groundwater flows into a channel along the highwall (constructed similar to Method 1) and flows down-dip through a porous gravel (or on-site rock) medium.

Factors that should be considered for sites where drains are proposed

  • All drain outlets should be designed with a "water trap" near the outlet to prohibit oxygen from entering the site through the drains.
  • Minimally, the discharge from drains should be monitored quarterly for quantity and quality. This will give an indication of how much groundwater is being intercepted and whether or not the intercepted water is being influenced by mine spoil.
  • Reclamation should be conducted rapidly since sites with highwall drains often have marginal overburden quality (near neutral or slightly acidic).
  • Dual highwall drains may be useful for large sites with significant infiltration from precipitation.

Porous Envelope: No Data

References:
http://handbooks.btcv.org.uk/handbooks/content/chapter/828, accessed December 2003
http://www.createalandscape.com/Houston%20Drainage.htm, accessed December 2003
http://www.dur.ac.uk/~des0www4/cal/dams/emba/seep.htm, accessed December 2003
Harry R. Cedergren, 1989, Seepage, Drainage and FlowNets, Wiley- Interscience Publishers, pp 465
http://www.dep.state.pa.us/dep/deputate/minres/districts/cmdp/chap16.html, accessed January 2004



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