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every one today we're going to belooking at cones of depression staticwater levels pumping water levelsdrawdown a whole bunch of differentconcepts and terminology that I'd liketo run through but basically all happensas a result of pumping water from anaquifer okay so here we have my littlediagram of an aquifer and a well so thiswhite thing is our well down here inthese black slots that's our screen okayso that's where water enters the wellhere we have our aquifer here we haveour water table there and here's thewater inside the aquifer so the firstthing we need to define and look at iswhat's called the static water levelokay let me write that down becausethat's an important concept static waterlevel and the static water level is theelevation of water in that aquifer whennothing is happening to that aquiferokay nothing is getting pumped outnothing is getting put in it's just thenormal natural elevation of water inYaqui fur okay I like to point out thatthe static water level is the sameoutside of the well as it is inside okaythere's no difference there and that'sbecause this well is open to thisaquifer through the screen and water canenter into the well through that screenand and kind of balance out at thestatic water level so now let's look ofwhat happens once we turn on the pumpthat's inside this well and startpumping water out of the aquifer throughthe well so the first thing that's goingto happen is that this water levelinside of the well is going to dropright because it's closest to the pumpso that's going to drop down to somelevel maybe right there and eventuallyit'll stabilize and water from theoutside of the well in the aquifer isgoing to enter the well through thatscreen right we're going to draw waterfrom the aquifer into the well once westart pumpingand initially water is going to comefrom all directions in this aquifer fromup top here down and then from the sidesand so the further away we are from thewell the less affected the water isgoing to be so the water maybe righthere is not as affected as it is righthas the water right here okay the waterright here is going to be moving quickright into that well the water out heremay be moving but it will be moving alot more slowly and how much the waterhere is affected depends on a few thingsthat we'll get into eventually okay solet's say we pumped on this well wepulled the water down into the well andwe've seen the water level inside thewall our static water level inside thewall dropped and the water level outsideof the wall is going to drop - okay andwe're going to form what's called a coneof depression okay and it's going tolook like this okay this is our cone ofdepression and let's write that down -because that's an important conceptand so this colorpression takes on the shape because likeI said earlier the water closest so wellis more affected than water further outfrom the well okay so water right hereis going to be moving faster towards thewell than it is out here and I thinkit's easy to to intuitively think thatwater right here is going to be greaterit's going to be more affected thanwater out here right I mean it's closerto the well so you just intuitively youcan figure out that that's the case butlet's do a little I'm going to show youwhy that is I'm going to get all rid ofthat stuff right now and start newcolors here okay so imagine imagine soremember this is a three dimensionalsituation right we got a two-dimensionalrepresentation of it this is in threedimensions in real life right so imagineso this this well is a cylinder rightnow imagine some imaginary cylindersoutside of the well in the aquifer okayso imagine we have a cylinder right1there and then imagine we have a larger1cylinder out here and imagine where1we're going to pump water from these1cylinders okay and they're imaginary1obviously but we're just creating some1some boundaries that we can think about1here let's call this guy cylinder one1and we'll say well say it's volume one1okay because we're going to imagine the1volume of this cylinder of this1imaginary cylinder and we'll call this1volume to the volume of this imaginary1cylinder - okay so these is easy to see1that the smaller cylinder is a smaller1volume than volume two right then the1the volume of cylinder two it's less1than the volume of cylinder two1if you imagine pumping water from each1of these cylinders which one is going to1empty first it's going to be the smaller1volume right it's going to be the1smaller cylinder because the smaller1volume of water and it will it'll empty1quicker because it's smaller volume1makes sense right and that's why this1cone of depression forms is because in1the first cylinder the water is going to1be drawn down much quicker and so the1water in that cylinder is going to empty1so you're gonna you're going to create1this curve there of where the water is1being drawn down and then out here it's1going to happen eventually maybe but1it's going to take a lot longer to get1there so that's why you create this cone1of depression okay hopefully that made1sense not too confusing let's go back to1our our drawing here and we're going to1define a couple other important points1okay so we've we've labeled the static1water level we've labeled our color1depression here another point we need or1another term that we needed to fine is1what's called our pumping water level1you can probably surmise what that is1right now right it's going to be the1water level inside of the well so it's1going to be right there when we're1pumping the well and it's going to be1the the equilibrate level inside the1wall so it's not going to be right after1we turn the pump on it's going to be1once it stabilizes right because the1water level inside the wall is going to1drop as we're pumping and eventually1it'll reach some stable point right1there and that stable level is called1the pumping water level okay so if the1static water level which was up here1before we turn the pump on and then we1have the pumping water level which is1down here after we pumped the well and1we've reached some sort of stable point1and the difference between these two1levels is what we call drawdown let me1write that down too1so drawdown is a pretty self-explanatory1name I think it's the amount of water1elevation that gets drawn down inside1the well after pumping for a period of1time at which point the pumping water1level is established and drawdown is an1important concept because it determines1how much water we can pump out of this1well okay because we can't have the1drawdown go past our pump because then1we won't be pumping water anymore okay1one other term I want to define here so1I think I'll call it good for this video1because we might get into I might be1laying a little too much information on1you but it's going to be called the1radius of influence and it's related to1the cone of depression and another1self-explanatory name I think it's just1the radius that the the cone of1depression reaches out to from the well1okay1three days of influence so it's how far1out the water table is going to be1affected by our pumping1makes sense it's just a radius from the1well to the edge of the corner1depression okay so I think this is a1good stopping point I don't want to1bombard you with too much information1here but in the next video we're going1to be talking about the coma depression1a little more and how far out it can1reach and how certain properties of the2aquifer and pumping rates and some other2things determine how far out this kind2of depression will reach so I'll put2that video in the comment section if you2found this useful go ahead and like the2video and subscribe to the channel and2I'll see you the next one

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Guide Groundwater FAQs

Hit on answers to listed questions about Guide Groundwater. Discover the most ordinary topics and more.

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Does gargling with saltwater replicate the effect of mouthwash and prevent the bacteria in the gums from coming out and forming plaque? How long can saltwater provide an environment that is hostile to bacteria?

The bacteria in the mouth survives on food particles left out in the mouth. A good wash with water will rinse off most of it and that alone can slow down the formation of plaque. The salt water kills the bacteria by sucking the water out of them, provided the salt concentration is sufficient. If you gargle with salt water with enough concentration and keep it on the mouth long enough for the bacteria to get dehydrated and die, then you can achieve a bacteria free mouth. The salt water can provide a hostile environment till the time the salt water is in the mouth. In practice, this doesn't happen. Some bacteria will escape, some gets into the mouth from the surroundings and in a few hours, the mouth will be full of them. Yes, the gargling will remove the food particles and reduce the activity of the bacteria which in turn helps the tooth. Gargling with salt water is definitely not a substitute for mouthwash.

What does the static level of a well mean?

I don't think they are the samething. I have a idea on how to make using freenet more difficult to be tracked. Tor and freenet can be combined to make you more safe. We need a trusted and powerful enough computer to run two virtual machines(VM). The first virtual machine uses host only network and run freenet on it. The other one run tor on it. The second VM has two network of host only and Internet access. The firewall should be configured that only tor is allowed to access the Internet. Then the freenet has to connect via tor. That means the attacker has to break tor and freenet to find you.

What is a ground level well?

A2A… From what I have seen about vertical antennas, the ‘ground plane’ antenna has 1/4 wave radials. You get a better match when they droop. All the regular designs have three radials but I saw somewhere that research showed that only one was really necessary. I think it gave a slight directive advantage in the direction of the radial. Tri-band verticals that cover 6m only ever have one radial loaded for 6m and I have seen (on the web) a page that describes how much better a commercial model worked with a full size 1/4 wave element instead of a loaded one. At ground level you don’t really need radials do you? Why not install a proper big earth mat and do the ‘ground plane’ business properly, for all bands. 73 de G4TRN

What is a groundwater well?

I will answer it in reverse . Traditional well in villages extracts water from adjoins areas of influence and stores it inside the well , which has a base which doesn’t have any fault/ crack to let water deep. It’s generally founded on hard rock below and water seeps into from around . Now with continuous extraction this water level goes down because of over drawl than the capacity of acquifer( acquifer is water bearing zone/ depth / band.)Now there are 2 ways to add / augment the capacity of acquifer . Manually and automatically automatically thru the process of rain water seeping into from ground and the other by diverting rain water into a borehole drilled ( recharge well) upto the acquifer depth. The rain water enters the acquifer and raises water level , called water table in engineering terminology.

Can you dig a well anywhere?

In many cases, they didn’t! Then again, the prairie water table wasn’t too deep, either, so, just find a low spot near a pot-hole pond & start drilling. Even so, there weren’t many natural springs or artesian wells & the water had to be pumped up, hence (from Siting Your Windmill ): The windmill water pump. A small aside: In the mid ‘30s, a ship approached Bahrain Island with a US based Geologist. His job was to site one of the first Oil Fields on the Bahrain Dome for exploitation. As the boat approached the island, he looked across the waters of the Gulf to Dahrahn & said, “There’s an even bigge Continue Reading

What are the 3 zones of groundwater?

I will interpret this question as “what are the two major types of groundwater aquifers?” The more commonly-known type is called an alluvial aquifer, which consists of water that resides in the ground beneath plains and river valleys. Groundwater in these aquifers resides in the void spaces that exist between gains of sand, gravel, cobbles, silts, and clay. The most simplified version of this type aquifer can be thought of as a bathtub full of sand, partially filled with water. If you stick a straw in, you can suck out water. Alluvial aquifers are reliable over large distances and are generally predictable in terms their location/depth and yield. Because they are most often so readily accessible to farmers, they tend to be overdrawn. The other, more complicated type of groundwater aquifer is a fractured rock aquifer, or bedrock aquifer. This type of aquifer underlies hills and mountains, as well as alluvial aquifers. Groundwater in this type of aquifer resides within fractures and fault zones in the rock. Water that exists in rock fractures flows more freely than water in an alluvial aquifer, but the location, extent and pervasiveness of fractures are very difficult to predict, and can be more readily depleted. The best bedrock aquifers are those where fractures in the rock intersect, creating a regional network of fractures. Wells in bedrock aquifers can perform very differently even when spaced very close together. It can often times be the luck of the draw to intersect a good fracture zone. In the image below[1] , the alluvial aquifer is shown in light grey and blue, whereas the bedrock aquifer is shown in dark grey. The essential difference is between water filling spaces between grains of sand/gravel/silt/clay (alluvial aquifer), and water filling the spaces between fractures (bedrock aquifer). Footnotes [1] Groundwater Conservation | Watershed Watch Salmon Society

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