Showing posts with label Aquifers. Show all posts
Showing posts with label Aquifers. Show all posts

Wednesday, January 20, 2021

COLIFORM “PRESENT” - How to Fix it - Coliform bacteria do not occur naturally in most aquifers. Fractured or creviced bedrock aquifers that are close to the surface are the exception. Be aware that there are three different groups of coliform bacteria; total coliform, fecal coliform and Escherichia coli (E. coli) each has a different level of risk. Keep in mind that coliform bacteria do not always show up in every sample. They can be sporadic and sometimes seasonal when they occur in a water supply. If your water is contaminated with coliform but not fecal coliform or E. coli, don't panic. You have a nuisance bacteria problem and the source may be infiltration from the surface from rain or snow melt. Typical causes are improperly sealed well cap, well repairs performed without disinfecting the well, failed grouting or surface drainage to the well. If your well had coliform bacteria present you should shock chlorinate the well, repack the soil around the well pipe to flow away from the well and replace the well cap. Then after at least two weeks and the next big rainstorm retest the well for coliform. If coliform bacteria is still present then a long-term treatment should be implemented: using UV light, ozonation, or chlorine for continuous disinfection. Coliform bacteria are commonly found in soil, on vegetation, and in surface water. Some coliform bacteria strains can survive in soil and water for long periods of time. Coliform bacteria will not likely cause illness.

......................................................................................................................................................................................................................................................................................................................................................................................

Coliform “PRESENT”

How to Fix it

.

Coliform bacteria do not occur naturally in most aquifers. Fractured or creviced bedrock aquifers that are close to the surface are the exception. Be aware that there are three different groups of coliform bacteria; total coliform, fecal coliform and Escherichia coli (E. coli) each has a different level of risk. Keep in mind that coliform bacteria do not always show up in every sample. They can be sporadic and sometimes seasonal when they occur in a water supply.

Elizabeth Ward

 


This spring in the well water clinic we run each year we found 25 wells out of 114 that had coliform "PRESENT."

On a state level, the occurrence of coliform is higher.

Of the approximately 7,000 households that participated in the Virginia Household Water Quality Program clinics from 2007 to 2015 they found that 41% of the wells had coliform bacteria, and 9% had E. coli bacteria.

Though the 7,000 households may not be representative of all private drinking water wells in Virginia, it is the largest database on private drinking water wells available.

It is safe to say that coliform contamination is widespread. 

If your water is contaminated with coliform but not fecal coliform or E. coli, don't panic.

You have a nuisance bacteria problem and the source may be infiltration from the surface from rain or snow melt.

Typical causes are improperly sealed well cap, well repairs performed without disinfecting the well, failed grouting or surface drainage to the well.

If your well had coliform bacteria present you should shock chlorinate the well, repack the soil around the well pipe to flow away from the well and replace the well cap.

Then after at least two weeks and the next big rainstorm retest the well for coliform.

If coliform bacteria is still present then a long-term treatment should be implemented: using UV light, ozonation, or chlorine for continuous disinfection.

These systems can cost up to $2,000 installed.

If your well test PRESENT for coliform standard protocol is:

1.    Carefully check the well and water system for points of contamination. Make sure you have a sound and secured sanitary well cap and that the soil around the well is packed to drain water away from the well. 

2.    Then treat the well and plumbing system with chlorine for 12-24 hours to disinfect system (the 12-24 hours is essential). Then flush the chlorine from the system- not to your septic system. Make sure that this is done correctly

3.    Retest the water after the chlorine has left the system in about 10 days to two weeks. If coliform bacteria is “ABSENT” you’re done. If not, then it is time to install a long term disinfection system. (UV light or continuous chlorination)

In an existing well system that formerly was bacteria free look for these defects:

·          A missing or defective well cap and check seals around wires, pipes, and where the cap meets the casing may be cracked, letting in contaminants. 

·         Contaminant seepage through the well casing - cracks or holes in the well casing allow water that has not been filtered through the soil to enter the well. This seepage is common in the wells made of concrete, clay tile, or brick. This can also happen to a steel pipe well that was hit by a piece of equipment such as a car, snow blower, lawn tractor or mower or that has rusted. 

·         Contaminant seeping along the outside of the well casing - many older wells were not sealed with grout when they were constructed or the grouting has failed. Check the grouting carefully especially if water seems different after severe rains. 

·         Well flooding - a common problem for wellheads located below the ground in frost pits that frequently flood during wet weather. 

Coliform bacteria are commonly found in soil, on vegetation, and in surface water.

Some coliform bacteria strains can survive in soil and water for long periods of time. Coliform bacteria will not likely cause illness.

Coliform bacteria do not occur naturally in most aquifers. Fractured or creviced bedrock aquifers that are close to the surface are the exception.

Be aware that there are three different groups of coliform bacteria; total coliform, fecal coliform and Escherichia coli (E. coli) each has a different level of risk.

If your water is contaminated with coliform but not fecal coliform or E. coli, then you have a nuisance bacteria problem.

Bacteria washed into the ground by rainfall or snowmelt are usually filtered out as water seeps through the soil, so properly constructed water wells do not typically harbor Coliform bacteria.

However, coliform bacteria can persist within slime formed by naturally occurring ground water microorganisms.

The slime (or biofilm) clings to the well screen, casing, drop pipe, and pump and may even invade filter systems.

Disturbances during pumping or well maintenance can cause the slime to dislodge, releasing the coliform bacteria.

Keep in mind that coliform bacteria do not always show up in every sample. They can be sporadic and sometimes seasonal when they occur in a water supply.

You should not continue drinking water contaminated with coliform, either boil the water drink bottled water until you disinfect your well.

Bring the water to a rolling boil for one to five minutes (the higher the elevation the more time is necessary) to kill the bacteria.

You may also want to consider using bottled water as a temporary drinking and cooking water source.

You may have received a total coliform count. This gives you a general indication of the sanitary condition of a water supply and extent of the problem.

Bacteria can be introduced into a new well during construction and can remain if the water system is not thoroughly disinfected and flushed.

Well construction defects such as insufficient well casing depth, improper sealing of the space between the well casing and the borehole, corroded or cracked well casings, and poor well seals or caps can allow surface water or insects to carry coliform bacteria into the well.

These problems are common and the most likely source of the coliform bacteria contamination.

Unplugged abandoned wells can also carry coliform bacteria into deeper aquifers.

Since bacterial contamination cannot be detected by taste, smell, or sight, all drinking water wells should be tested at least annually for Coliform bacteria.

Elizabeth Ward was awarded an MBA from the University of Pittsburgh and an MS ChE from NYU Tandon School of Engineering, worked as a chemical engineer for both the US EPA in DC, and at DuPont before working in finance and then becoming consultant with Washington Advisors and is the author of "The Lenders Guide to Developing an Environmental Risk Management Program." Elizabeth retired from Washington Advisors and began her volunteer career and served 10 years as the Treasurer of the Prince William Soil and Water Conservation District.

https://greenrisks.blogspot.com/2018/05/coliform-present-steps-to-take.html


You might also like:


Owning A Home With A Well

CLICK HERE . . . to view . . . 

https://puricare.blogspot.com/2020/06/owning-home-with-well-if-youre.html

...........................................................................................................................................................................................................................................................................................

Well Disinfection

CLICK HERE . . . to view . . . 

https://puricare.blogspot.com/2020/01/well-disinfection-keep-children-and.html

...........................................................................................................................................................................................................................................................................................

Backpacking Water Treatment

CLICK HERE . . . to view . . . 

https://puricare.blogspot.com/2021/01/backpacking-water-treatment-options.html

...........................................................................................................................................................................................................................................................................................

Food Contaminated With E. Coli

CLICK HERE . . . to view . . . 

https://puricare.blogspot.com/2020/05/food-contaminated-with-e-coli-how-can-i.html

...........................................................................................................................................................................................................................................................................................

E. Coli is Found in the Human Digestive Tract

CLICK HERE . . . to view . . . 

https://puricare.blogspot.com/2020/05/e-coli-is-commonly-found-in-human.html

...........................................................................................................................................................................................................................................................................................

Coliform Bacteria

CLICK HERE . . . to view . . . 

https://puricare.blogspot.com/2019/11/coliform-bacteria-organisms-known-to.html

...........................................................................................................................................................................................................................................................................................

E. Coli Contamination Found In Tap Water

CLICK HERE . . . to view . . . 

https://puricare.blogspot.com/2017/03/e-coli-contamination-in-tap-water-e.html

...........................................................................................................................................................................................................................................................................................

Drinking The Water Directly From A Private Well

CLICK HERE . . . to view . . . 

https://puricare.blogspot.com/2016/10/drinking-water-from-private-well.html

...........................................................................................................................................................................................................................................................................................

Did God Make Harmful Parasites in the Beginning?

CLICK HERE . . . to view . . . 

https://puricarechronicles.blogspot.com/2021/01/blog-post_76.html

...........................................................................................................................................................................................................................................................................................

Pestilence And Disease On A Global Scale

CLICK HERE . . . to view . . . 

https://puricarechronicles.blogspot.com/2020/05/pestilence-and-disease-on-global-scale.html

 

Friday, January 15, 2021

OVER-PUMPING OF UNDERGROUND AQUIFERS - How Over-Pumping of Underground Aquifers Can Cause Land to Sink - Sucking water from aquifers can cause land to compact over time, often lowering it hundreds of feet in elevation. Specifically, in reference to our drinking water, around half of the US population gets their drinking water from either public or private wells. Water wells are used on a massive scale. They suck water from underground aquifers for use in agriculture or for drinking water. Water is, after all, essential to life, but many civilizations have developed in regions of the world that don't have access to sufficient surface freshwater. Issues arise when the amount of water pumped out of the aquifers is greater than the amount of water flowing into the aquifers. When over-pumping occurs, large swaths of soils underground that previously were saturated with water are now left dried out permanently. All the static and dynamic forces from the land and rock above start adding up and eventually that now-dry soil starts compacting down and down. While this may not seem like a big deal on a small scale, what we've seen in California is the dropping of the surface elevation over a period of years, often by hundreds of feet or meters. This dropping of the ground level is an aspect of a principle called land subsidence. Land subsidence can occur when significant portions of groundwater are pumped out or removed from underground rock and soil.

..........................................................................................................................................................................................................................................................................................................................................................................

Over-Pumping of Underground Aquifers

How Over-Pumping of Underground Aquifers Can Cause Land to Sink

Sucking water from aquifers can cause land to compact over time, often lowering it hundreds of feet in elevation.

By Trevor English



If you're reading this, chances are you don't really have to think about where your drinking water is coming from, how your food was grown, or what effects such processes have had on the environment.

Specifically, in reference to our drinking water, around half of the US population gets their drinking water from either public or private wells.

Water wells are used on a massive scale. They suck water from underground aquifers for use in agriculture or for drinking water.

Water is, after all, essential to life, but many civilizations have developed in regions of the world that don't have access to sufficient surface freshwater.

Take, for example, California and much of the southwestern United States. While this region is one of the most densely populated in the country, it also happens to be one of the most water-scarce.

California has a massive agricultural industry too, meaning the state requires a significant amount of water on a daily and seasonal basis.

For the most part, the states' water has historically come from wells drilled that pump out freshwater from confined and unconfined aquifers under the surface.

This is a fairly common practice globally, but issues arise when the amount of water pumped out of the aquifers is greater than the amount of water flowing into the aquifers.

When over-pumping occurs, large swaths of soils underground that previously were saturated with water are now left dried out permanently.

All the static and dynamic forces from the land and rock above start adding up and eventually that now-dry soil starts compacting down and down.

While this may not seem like a big deal on a small scale, what we've seen in California (and other parts of the world too) is the dropping of the surface elevation over a period of years, often by hundreds of feet or meters.

This dropping of the ground level is an aspect of a principle called land subsidence. Let's take a closer look at just what is occurring.

What is land subsidence?

Land subsidence can occur when significant portions of groundwater are pumped out or removed from underground rock and soil.

The previously water-saturated rock and soil, which is now dry, start compressing under the forces of the rock above it.

Land subsidence is a fairly slow process, and is not generally noticeable on a day to day or minute to minute basis, in the way that says, an earthquake would be.

Localized subsidence is also the principle that describes why a sinkhole or a pothole might occur, only in these cases, it's far more localized land subsidence than the kind that would drop an entire region's elevation.

While dropping the surface elevation in a region may not seem like a big deal, it's actually a rather costly one.

In theory, the dropping of the ground level is fine if it occurs evenly everywhere, but that's not the case.

Land subsidence is a highly variable process, based largely on the soil makeup under the surface.

If one area is comprised mainly of soft clay and the other is mainly of silt, the two areas are going to compact at different rates, even if they took up the same volume when saturated with water.

Since soils are made up of different components and have different shapes and sizes of particles, this also means that different soils can take up various amounts of water.

In gardening, this is one reason why you might buy specialty potting soil – to help the soil retain more or less moisture.

In geology, these different absorption rates impact how engineers design building foundations and wells for underground aquifers.

Back to the core principle here, land subsidence is a big issue because it causes the ground level to sink at highly variable and uneven rates.

When structures are present on the surface, the movement can be enough to crack foundations, collapse bridges, crack underground pipes, and otherwise wreak havoc on civil infrastructure.

Humans have a pretty hard time visualizing something that happens over the span of years though, so I find that when learning about land subsidence, the most effective thing you can do is look at pictures that document its effects.

Perhaps one of the most famous is that of the subsidence that occurred in the California Valley over the span of five decades.

As a warning, this image is going to require some scrolling, but it hopefully underscores just how substantial land subsidence can be.

After seeing that, you hopefully have some grasp on just how substantial land subsidence from over-pumping of aquifers can be.

One might next wonder how this can be tracked and prevented.

While we won't go into that too much in this article, the short answer is that governing bodies track the water levels in wells across a region to monitor whether there is more or less water.

If signs of overpumping are starting to be seen, engineers can either keep pumping and deal with the effects of subsidence, or find another source for water.

The USGS Active Groundwater Level Network includes about 20,000 wells that have
 been measured by the USGS or USGS cooperators at least once within the past 13 months.
The animation shows a daily snapshot of water-level statistics in the network for July 2015,

The gif below is a compilation of USGS well data across the US, indicating water levels in their well network.

This type of data is one of the tools engineers use to figure out how underground water is flowing, refilling, and otherwise behaving.

Engineers will also utilize tools like compaction recording devices to measure the change in sediment layer thicknesses underground.

These tools, rather than measuring water level, allow engineers to measure the soil effects from well pumping in a given area.

The figure below does a pretty good job explaining how this works.

The harmful effects of over-pumping

We've talked a little about how harmful over-pumping can be to buildings and infrastructure, but this isn't the only issue with overpumping, nor have we discussed the full scope of the infrastructure issues that arise.

Land subsidence has many core problems, most of which can be summed up concisely like this – land subsidence can cause:

o  Changes in elevation and slope of streams and surface water systems

o  Damage to infrastructures like roads, bridges, pipes, levees, and sewers

o  Damage to surface buildings

o  Failures of wells

o  The intrusion of chemicals from agriculture

One of these problems is a change to naturally occurring geography, three are changes to infrastructure, and the last is the degradation of water quality.

Let's focus on the change to geography first.

If subsidence changes the path or elevation change across a stream, it can increase its flow rate, causing more erosion in a given area, which can make it harder for certain types of fish and plants to survive, and all of this, in turn, could impact the surrounding ecosystem and even human habitation.

Changes in geography from land subsidence can affect coastal regions too. A house once built far away from high tide elevation may suddenly find itself dangerously close to the water.

Keep in mind this effect is completely different from changes in tide levels caused by climate change.

Going back to the initial list of problems, we've already spent a decent amount of time going over how changes to the ground might impact, damage, or destroy surface and subsurface infrastructure, so I'm mostly going to skip over those effects for further explanation.

What is a new topic though, is the discussion of how land subsidence can actually pollute subsurface water.

Specifically, overpumping from wells can cause concentrations in groundwater of pollutants like arsenic to skyrocket.

Arsenic is a naturally-occurring chemical in nature. Over time, arsenic is transported through rivers and deposited into clay.

This has occurred for millions of years and over time, these clay layers get pushed deeper and deeper into the earth's crust.

What has ended up occurring is a large arsenic concentration in deep clay structures, usually far deeper than wells would ever pump.

However, when wells are overpumped and the soil on top is drained of water, the well starts pulling water from the fine clays underneath, which can have high arsenic concentrations, bringing the arsenic along with it.

This increased arsenic concentration can then pollute crops and drinking water.

Even low levels of arsenic, such as 10 milligrams per liter (8.3 pounds per gallon), are harmful and can cause increased rates of cancer, heart disease, and diabetes.

At the end of the day, land subsidence from over-pumping of subsurface aquifers is a major issue in water-starved regions across the world.

It's also an issue that's not easily solved since, first and foremost, societies need water.

It can be very difficult to switch to less water-intensive crops or growing methods, and you can't just tell people not to drink water or grow crops.

Land subsidence is just one of the fascinating issues that civil and environmental engineers work to solve on a daily basis, and it's one that crucial to the future of many regions across the world.

Trevor English

Writer

Trevor is a civil engineer (B.S.) by trade and an accomplished writer with a passion for inspiring everyone with new and exciting technologies. He is also a published children’s book author and the producer for the YouTube channel Concerning Reality.

https://interestingengineering.com/how-over-pumping-of-underground-aquifers-can-cause-land-to-sink


You might also like:


Aquifers

Underground Stores of Freshwater

CLICK HERE . . . to view . . . 

https://puricare.blogspot.com/2019/12/aquifers-underground-stores-of.html

............................................................................................................................................................................................................................................................................................

The Science of Sinkholes

CLICK HERE . . . to view . . . 

https://puricare.blogspot.com/2016/06/sinkholes-sinkhole-is-depression-in.html

............................................................................................................................................................................................................................................................................................

Groundwater, Aquifers and Water Movement

CLICK HERE . . . to view . . . 

https://puricare.blogspot.com/2016/08/groundwater-occurs-in-saturated-soil.html

............................................................................................................................................................................................................................................................................................

Sinkholes In Guimaras

CLICK HERE . . . to view . . . 

https://puricare.blogspot.com/2016/06/sinkholes-in-guimaras-subsidence-due-to.html

............................................................................................................................................................................................................................................................................................

Saltwater Intrusion

CLICK HERE . . . to view . . . 

https://puricare.blogspot.com/2021/01/saltwater-intrusion-growing-threat-to.html

............................................................................................................................................................................................................................................................................................

Protecting Drinking Water from Saltwater Intrusion

CLICK HERE . . . to view . . . 

https://puricare.blogspot.com/2020/12/protecting-drinking-water-from.html