Are Water Restrictions Coming for You?

Last Friday, the Fauquier County Water and Sanitation Authority (FCWSA) implemented mandatory water restriction rules, due to the active Drought Warning Advisory issued by the Virginia Department of Environmental Quality.

The mandatory rules target outdoor water consumption for all customers on the public FCWSA water systems to preserve water pressure and fire protection services. Residents relying on private wells are strongly encouraged to voluntarily practice the same conservation measures.

The mandatory restrictions ban or strictly limit the following activities:

• Lawn Watering: The use of sprinklers or irrigation systems is prohibited.
• Vehicle Washing: Washing cars, trucks, or trailers at home is banned, except at dedicated commercial facilities that use water recycling systems.
• Pool Filling: Filling empty swimming pools or wading pools (or those less than three-quarters full) is prohibited.
• Surface Cleaning: Washing down driveways, sidewalks, parking lots, or exterior building structures is barred unless required for health or safety.
• Decorative Elements: Operating non-essential water amenities like fountains, waterfalls, or reflecting ponds is banned unless required to sustain aquatic life.

Caroline County has also issued mandatory water restrictions. Due to extreme drought conditions straining their groundwater supply, county officials elevated local emergency rules to Level 3 Mandatory Restrictions.

The broader D.C. metropolitan area remains under a regional Drought Watch, meaning that local jurisdictions rely entirely on voluntary cutbacks to protect the Potomac River basin. If you recall at the beginning of June, the Metropolitan Washington Council of Governments (COG) put a Drought Watch into effect due to the unusually dry conditions that are expected to persist despite recent rainfall. The regional Drought Watch applies to nearly six million residents across the District of Columbia, suburban Maryland, and Northern Virginia the water saving measures requested are voluntary.

Fairfax Water & Fairfax City

Fairfax Water emphasizes optimizing daily household routines to keep backup reservoirs full:

·         Indoor: Shorten showers to under 5 minutes, turn off faucets while brushing teeth or shaving, and fix plumbing leaks immediately (especially running toilets).

• Appliances: Only run dishwashers and laundry machines when fully loaded.
• Outdoor: Minimize the watering of lawns or shrubs, use a broom instead of a hose to clear driveways, and avoid home car washing. Loudoun Water & Town of Leesburg

Loudoun Water and the Town of Leesburg ask residents to fundamentally shift outdoor water usage to slow down the drought's impact:

• Lawn Care: Suspend or heavily restrict routine lawn irrigation; let established grass go dormant in the dry weather.
• Targeted Watering: Prioritize root systems of newly planted trees or essential shrubs using a slow drip to prevent runoff.
• Vehicle Washing: Skip home vehicle or boat washing entirely, or substitute with commercial recycling car washes.

Prince William Water

Prince William Water focuses heavily on strict monitoring of outdoor demands while supply in the Potomac remains adequate:

• Landscaping: Actively monitor and decrease the frequency of plant and shrub watering.
• Hardscape Cleaning: Heavily discourage hosing down patios, sidewalks, and siding, requesting sweeping instead.
• Kitchen Habits: Run the faucet only when actively scrubbing dishes if washing by hand.

Town of Purcellville

Because the Town of Purcellville operates on an independent groundwater/well network, they remain at a localized Drought Warning level despite lifting mandatory restrictions. They request the most aggressive voluntary pullbacks in the area:

• Strict Conservation: Voluntarily cease all non-essential outdoor water usage.
• Peak Shaving: Minimize any essential appliance use during peak early morning and late evening hours to protect community system pressure

DC Water Voluntary Guidelines

The utility urges consumers to practice "wise water use" through minor adjustments to daily household routines:

• Shorter Showers: Keep daily showers under 5 minutes.
• Faucet Habits: Turn off the tap while brushing teeth, shaving, or scrubbing dishes by hand.
• Smart Outdoor Watering: Limit unnecessary watering, and only water yards during the early morning or evening to minimize evaporation.
• Full Laundry/Dish Loads: Delay running appliances until they are completely full.
• Proactive Leak Checks: Inspect toilets, faucets, and exterior hoses for hidden leaks and patch them immediately

WSSC Water Voluntary Restrictions (Current)

WSSC Water has adopted the regional "Wise Water Use" guidelines under the current Drought Watch. They ask customers to:

• Outdoor:

o    Limit lawn watering and stop if it rains.

o    Use a broom, not a hose, to clean driveways, sidewalks, and patios.

o    Use commercial car washes that recycle water instead of washing vehicles at home.

o    Water flowers and shrubs with a hand-held hose or watering can rather than automated sprinklers.

• Indoor:

o    Keep showers to under 5 minutes.

o    Turn off faucets while brushing teeth or shaving.

o    Only run dishwashers and washing machines with full loads.

o    Check for and repair silent leaks, especially in toilets (a major source of wasted water).

 Because WSSC, Fairfax Water, Prince William Water, Loudoun Water, and the Town of Leesburg all share the Potomac River as their primary water source, they coordinate their restriction levels together through the Metropolitan Washington Council of Governments. They will move to mandatory restrictions only when the region escalates to a Drought Emergency. The trigger for a drought emergency is: Critical water shortage where backup reservoirs are dangerously low and there is an imminent risk of not meeting essential public health and safety needs (fire protection, drinking water).

EPA Proposed Changes to PFAS Drinking Water Rules

EPA Proposed Changes to PFAS Drinking Water Rules

In a May 18, 2026 press release, the U.S. Environmental Protection Agency (EPA) announced a proposed rule that would rescind the 2024 drinking water standards for PFHxS, PFNA, HFPO-DA (GenX chemicals), PFBS, and the hazard index for mixtures involving these PFAS.

• Written comments on the proposed rule are due by July 20, 2026.
• The public docket is available at www.regulations.gov under Docket ID: EPA-HQ-OW-2025-0654.
• The EPA will hold a virtual public hearing on July 7, 2026 to present information on the proposal and receive verbal comments.
• Registration is required to attend or speak, and the deadline to pre-register to provide public comment is July 1, 2026.
• Information and registration for the hearing are available here.
• The EPA will post the hearing agenda and list of pre-registered speakers by July 6, 2026.
• Questions about the hearing may be directed to PFASNPDWR@epa.gov.

The EPA is also proposing to extend the compliance deadlines for the PFOA and PFOS maximum contaminant levels (MCLs). The hearing on that proposal will be held sequentially with the PFAS rescission hearing.

In practical terms, the EPA is not simply revisiting these rules; it is proposing to revoke the existing 2024 enforceable limits for GenX, PFNA, PFBS, and PFHxS and begin a new review process that could take years. If finalized, those chemicals would return to an unregulated federal status during that period. At the same time, the compliance deadlines for PFOA and PFOS would be extended by two years.

Virginia's Response

Because Virginia public water systems must ultimately align with federal Safe Drinking Water Act standards, the Commonwealth is focusing on upstream sources of PFAS contamination. The Virginia Department of Environmental Quality (DEQ) is leading several initiatives under state legislation signed by Governor Spanberger on April 26, 2026.

• When the Virginia Department of Health (VDH) identifies a public water system that exceeds a PFAS threshold, DEQ must trace the contamination back to its source.
• DEQ may require suspected industrial facilities and manufacturers to self-report or monitor PFAS discharges for one year.
• Publicly owned wastewater treatment plants, airports, firefighting facilities, and industrial chemical users must test their effluent and discharges for PFAS and report the results to DEQ.

Related Virginia laws also expressly allow localities to require PFAS testing of sewage sludge, or biosolids, before those materials are applied to farmland as fertilizer. This matters because land application is one pathway by which PFAS can enter the food supply. Wastewater treatment plants do not destroy PFAS; instead, they concentrate these chemicals in solid residuals. When a municipal plant receives waste from sources such as chemical manufacturers, carpet producers, or facilities that used aqueous film-forming foam (AFFF), the resulting biosolids can contain elevated PFAS concentrations.

When biosolids with elevated PFAS are spread on fields, short-chain PFAS compounds can be taken up by crops such as corn and grains. Livestock that consume those crops or graze on sludge-amended pasture can then accumulate PFAS in their milk, fat, and organs. In several states—including Maine, Michigan, and Texas—this contamination has contributed to severe agricultural losses, including farm closures and the culling of herds.

COG Declares a Regional Drought Watch

The following is a news release from the Metropolitan Washington Council of Governments"

 Washington, DC (June 3, 2026) – A Drought Watch was put into effect today by the Drought Coordination Committee of the Metropolitan Washington Council of Governments (COG) following unusually dry conditions that are expected to persist despite recent rainfall. The regional Drought Watch applies to nearly six million residents across the District of Columbia, suburban Maryland, and Northern Virginia.

Officials stress that while there is currently an adequate supply of water in the Potomac River and backup reservoirs, residents and businesses are encouraged to practice wise water use by taking simple, voluntary steps to reduce water use and help protect the region’s water resources if dry conditions persist.

 

Here are some simple tips residents can use to limit indoor and outdoor water use:

 

INDOOR

• Reduce shower length to under 5 minutes;
• Turn off water while brushing your teeth/shaving;
• Wash only full loads of dishes and clothes; and
• Fix any plumbing leaks – especially toilets and faucets.

OUTDOOR

• Monitor watering lawns, plants, and shrubs;
• Sweep sidewalks and driveways (instead of using a hose); and
• Avoid washing your car or instead use a commercial car wash that recycles water.

The region’s last Drought Watch occurred between July 2024 to June 2025. This year, from March to April, the region experienced record-breaking high temperatures along with some periods of historically low streamflow levels. The Potomac River reached its lowest level during this time period, based on 130 years of data. In addition, the two-year precipitation deficit is almost 8 inches.

 

“Our region hasn’t seen extremely dry conditions like this in about two decades when local leaders and COG first established a drought response plan to support coordination and communication regionwide,” said Clark Mercer, COG Executive Director. “During the Drought Watch, we’re asking the public to help by incorporating simple, water-saving actions into their daily routines.”

 

A Drought Watch is an early advisory stage in the Regional Drought Response Plan. It is the level before the Drought Warning stage, when water restrictions would be encouraged. At the highest Emergency stage, jurisdictions and utilities may implement mandatory water use restrictions in a coordinated manner. Since the adoption of the regional drought plan in 2000, the region has not entered the Drought Warning stage.

“Due to years of planning and preparation, our water supply infrastructure is well-equipped to handle drought. Nevertheless, it makes sense for all of us to use water wisely to conserve this precious resource,” stated Michael Nardolilli, the executive director of the Interstate Commission on the Potomac River Basin (ICPRB). The ICPRB is monitoring the Potomac River flow daily and working with several federal agencies, regional partners, and area water suppliers to assess the situation in real time. The Potomac River supplies 78 percent of the drinking water for the region.

 

“We’re working closely with our regional partners to actively monitor conditions and protect our shared water resources,” said WSSC Water General Manager and CEO Kishia L. Powell. “While our water supply remains stable, now is a great time for all of us to practice wise water use. By making simple, voluntary changes in daily routines, our customers can save water and money.”

 

“The Washington Aqueduct stands fully ready and prepared to meet the operational demands of our region during these drought conditions,” said Washington Aqueduct General Manager Rudy Chow. “However, managing our shared water resources is a collective responsibility. We rely on the community’s awareness and voluntary actions to ensure long-term water resiliency for everyone.”

 

“While our region has an adequate water supply to meet demands, the public can make a difference during these dry spells by using water wisely,” said Fairfax Water General Manager Jamie Bain Hedges.

 

JURISDICTIONS IN THE COG DROUGHT WATCH:

 

District of Columbia

 

Suburban Maryland

Town of Bladensburg; City of Bowie; City of College Park; Charles County; City of Frederick; Frederick County; City of Gaithersburg; City of Greenbelt; City of Hyattsville; City of Laurel; Montgomery County; Prince George's County; City of Rockville; City of Takoma Park

 

Northern Virginia

City of Alexandria; Arlington County; City of Fairfax; Fairfax County; City of Falls Church; Loudoun County; City of Manassas; City of Manassas Park; Prince William County

The Impact of Development on Source Water and Groundwater Recharge

The water flowing from our taps doesn't originate at a treatment plant; it begins in our watersheds, specifically the upstream land of the greater Occoquan Watershed. When development occurs—such as paving and building within the watershed—we do more than alter the scenery. These actions fundamentally change how water moves through the landscape, how streams withstand drought, and how much pollution ultimately reaches the reservoir.

Development and Its Consequences

Every acre of forest and field that is converted into roofs, roads, and driveways reduces groundwater recharge and increases polluted runoff. This pushes our streams closer to drying up, causing gradual, cumulative, and eventually sudden destruction of our source water.

Currently, there is a proposal to amend the Comprehensive Plan for more than 200 acres west of Thoroughfare Road and south of John Marshall Highway. This proposal would change zoning from A-1 Agricultural to Planned Mixed Residential (PMR), permitting 97 detached homes, 56 attached homes, and the accompanying roads, parking lots, driveways, patios, and other impervious surfaces. Such changes are not neutral for the water supply; they directly impact the land that feeds our streams and, ultimately, the Occoquan Reservoir. It is not just this change it is the destruction of the watershed one comprehensive plan amendment at a time. 

Importance of the Bull Run Watershed

The Bull Run watershed is a vital part of the source-water system for the Occoquan Reservoir, which supplies drinking water to eastern Prince William County and much of eastern Fairfax County. The lower Bull Run area remains one of the most intact and least-disturbed sections of the watershed. Once these headwaters are fragmented and paved, we lose the natural infrastructure that maintains clean water, particularly during droughts. The issues observed in Little Bull Run are not isolated; they serve as a warning regarding the consequences of continued development in western and central Prince William for our drinking water supply.

Groundwater: The Invisible Essential

To understand the ongoing changes, it's important to discuss groundwater, which is invisible yet essential. Groundwater typically provides 30% to more than 50% of the annual flow for streams and rivers. This steady, slow-moving contribution is known as baseflow and acts like a "savings account," sustaining streams over time and providing flow during dry spells.

Drought and Its Effects

Prince William County and most of Virginia are currently experiencing severe drought. While the region usually receives about 44 inches of rainfall annually, last year was about 9 inches below average, and the first half of this water year saw roughly half the usual precipitation- about 13 inches below average. Despite a period of very wet years from 2018 to 2021, followed by near-normal rainfall with dry summers, recent summers have exposed weaknesses in the system.

Stream and Groundwater Dynamics

Streams in the Bull Run watershed are “gaining” streams, receiving direct groundwater supply. For groundwater to feed a stream, the water table must be higher than the stream’s water level, allowing water to seep through streambeds and banks. Excessive groundwater withdrawal or reduced recharge can sever this connection, turning perennial streams into seasonal ones.

Impervious Cover and Stormwater Runoff

As development increases impervious cover—such as roads, pavement, and buildings—the area available for rain and snow to infiltrate the ground decreases. Stormwater velocity and quantity rise, preventing infiltration and increasing flooding, which carries fertilizers, oil, grease, and road salt into rivers and streams. In the past six years, stormwater flooding has occurred adjacent to previously open areas of the county away from the shoreline.

Increased runoff volume and velocity lead to higher peak storm flows, causing flooding, soil erosion, and fast-moving water that carries contaminants. Reduced infiltration means less groundwater, which is essential for maintaining the base flow to streams and rivers feeding the Occoquan Reservoir during dry months.

Groundwater Recharge Trends

Groundwater in the Culpeper Basin is generally replenished annually through precipitation, but increasing impervious surfaces have altered this balance. In the past, water withdrawal matched recharge rates, ensuring adequate supply even during droughts. However, the region’s only nearby US Geological Survey groundwater monitoring well has shown a slow decline in water levels over the past decade and a half, despite varied rainfall conditions.

Watershed Response to Development

In Haymarket, the Bull Run Mountain Conservancy found that perennial streams such as Little Bull Run and Catlett’s Branch were dry during a dry August, with Catharpin Creek reduced to puddles. This was the driest period observed and may signal a new normal during dry times, highlighting how the watershed responds to recent development.

Reduced groundwater levels gradually transform perennial streams into ephemeral ones, disconnecting groundwater from surface water. Once development destroys watershed hydrology, restoration becomes extremely difficult. The Occoquan watershed is essential for regional drinking water, and groundwater is critical for streams and rivers.

Protecting Groundwater and Hydrology

Long-Term Watershed Changes

Development triggers immediate responses in a watershed, but significant ecological and physical changes take 20 to 50 years to fully emerge. Replacing 35–50% of forested areas with impervious surfaces permanently alters water movement. As impervious coverage increases, profound hydrological and ecological shifts occur over time.

Hydrological Alterations

• Runoff reaches streams more rapidly and in larger volumes, causing higher peak floods and more frequent flooding.
• Perennial streams begin to dry out or flow intermittently, eventually becoming ephemeral.
• Impervious surfaces prevent water from soaking into the ground, leading to dropping water tables and dry streams during summer.

Physical and Water Quality Changes

• High-velocity storm runoff causes severe bank erosion, incision, and blowouts, destroying aquatic habitats.
• Stormwater carries oils, heavy metals, road salts, and nutrients directly into waterways, bypassing natural filtration.
• Rainwater flowing over heated pavement raises stream temperatures, threatening aquatic life.
• Pavement, compacted lawns, and buildings prevent groundwater percolation, increasing land temperatures.

The cumulative effects observed now stem from building during the 1990s through 2007.

Recommendations for Protecting Source Water

• Treat the Bull Run watershed as source-water infrastructure—not as leftover land for development.
• Oppose Comprehensive Plan changes and rezonings that increase impervious cover in headwaters feeding Bull Run and the Occoquan system.
• Enforce stronger safeguards: limits on impervious cover, meaningful forest protection, groundwater-recharge preservation, and stormwater designs that mimic natural infiltration.
• Support acquisition and conservation easements for large, connected tracts in the watershed, because once developed, hydrology is permanently changed.

If the watershed continues to be treated as an empty canvas for growth, we risk actively destroying the source water for our regional drinking water supply, incrementally through rezoning, roads, and parking lots. By protecting infiltration, baseflow, and intact stream corridors now, we can safeguard the Occoquan for decades to come.

The time has come to Regulate Chemical AST's

 As of late Tuesday night, May 26, 2026, the emergency at the GKN Aerospace facility in Garden Grove has been resolved, and all evacuation orders have been lifted. According to news reports, The threat of a catastrophic explosion has been completely ruled out. A structural crack that naturally formed in the upper portion of the tank over the weekend served as a crucial fail-safe, safely venting the excessive internal pressure and naturally cooling the internal chemical. This was the best outcome of the situation.

The crisis in Orange County, California, began involving a 34,000-gallon aboveground storage tank (AST) holding highly volatile methyl methacrylate (MMA) at the GKN Aerospace facility in Garden Grove.  

An overnight internal temperature spike caused the tank to over-pressurize and off-gas vapors. Emergency mitigation completely stalled because the tank's drainage and mechanical valves were not working and "gummed up," preventing responders from pumping out the chemical or injecting neutralizing stabilizers. Having started my environmental career in 1978 helping to create RCRA this makes me insane. The area was evacuated for days. And to try and lower the tank temperature, emergency crews used unmanned high-volume water cannons (which were dousing the tank with over 1,200 gallons of water per minute). Trying to stabilize the tank’s temperature.

History of the Tank and Facility

While GKN Aerospace has operated the facility on Western Avenue since 2004, the chemical storage tanks on-site have been present since at least 1972, meaning parts of the physical infrastructure are over 50 years old.

The facility uses MMA to manufacture specialized, high-performance acrylic windscreens for military fighter jets. MMA is highly reactive and prone to dangerous exothermic (heat-generating) polymerizing reactions if not carefully stored and kept below 77 degrees Fahrenheit.

Inspection and Violation History

California officials have openly attributed this crisis to a systemic failure of safety redundancies and poor equipment maintenance rather than simple age-related decay. The facility has a documented history of oversight failures. Reports on file indicate that the facility has incurred 10 OSHA violations, including a specific citation for failing to maintain manufacturing machinery according to the manufacturer’s instructions.

The operator, GKN Aerospace,  paid nearly $1 million to settle environmental violations, highlighting a pre-existing history of compliance issues regarding hazardous materials handling.

Aboveground Storage Tank (AST) Regulations in California

Above Ground Storage Tanks  (AST) are not properly regulated in the United States. California, with some of the strongest AST regulations maintains a bifurcated regulatory framework depending strictly on whether they hold petroleum or hazardous non-petroleum chemicals and only bothers with petroleum products.

California's Aboveground Petroleum Storage Act (APSA) strictly regulates facilities storing 1,320 gallons or more of petroleum products (such as diesel, gasoline, or crude oil). Because methyl methacrylate is an industrial solvent/monomer and not a petroleum product, it falls entirely outside of the regulation’s jurisdiction.

Industrial chemical ASTs are instead regulated under California's Hazardous Materials Release Response Plans and Inventory law. Facilities holding hazardous chemicals above threshold quantities (55 gallons for liquids) must submit Hazardous Material Business Plan to the local Certified Unified Program Agency (CUPA)—typically a county environmental health department or a large city fire department that locally enforces state environmental and emergency management laws. The primary purpose of an HMBP is to provide immediate, accurate information to first responders (like firefighters and hazmat teams) during an emergency, ensuring they know exactly what chemicals are inside a building before they enter.

Because MMA is highly reactive and flammable, facility infrastructure is bound by Cal/OSHA standards (Title 8, Section 5189). This legally mandates mechanical integrity programs, meaning the facility is required to routinely inspect, test, and maintain critical process components—including piping, relief valves, and cooling systems—to prevent catastrophic failures. Clearly, this did not happen appropriately for a tank that is believed to be over 50 years old.

Relying solely on general Hazardous Materials Business Plans allows chemical aboveground storage tanks (ASTs) to bypass some of the engineering and safety mandates applied to petroleum tanks. California and the rest of the nation needs Chemical AST Regulations.   Stealing profusely from the CA Aboveground Petroleum Storage Act, and with the help of AI to examine AST regulations across the land, this is what needs to be done in California and elsewhere:

1. Mandatory Secondary Containment

Every chemical AST must have a secondary containment system to isolate spills and prevent environmental contamination.

• Volumetric Capacity: Containment basins must hold 110% of the single largest tank's volume, plus additional capacity to hold a 25-year, 24-hour rainfall event for outdoor tanks.
• Material Impermeability: Liners and concrete basins must be chemically compatible with the stored substance. For reactive monomers like methyl methacrylate (MMA), containment must feature non-porous coatings to prevent absorption and chemical degradation.
• Separation Defenses: Impoundment areas must segregate incompatible chemicals. Acids, bases, and highly reactive monomers cannot share a drainage basin to avoid accidental mixing and violent exothermic reactions.

2. Risk-Based Lifespan and Age Limitations

Because physical infrastructure degrades over time, tanks must face stricter regulatory hurdles as they age.

• Design Life Cap: Implement a mandatory 50-year structural lifespan cap for high-risk chemical ASTs. Beyond 50 years, tanks must either undergo complete shell replacement or pass a rigorous, destructive metallurgical evaluation to clear them for 5-year extensions.
• Fitness-For-Service (FFS): After 20 years of service, operators must conduct an API 579 Fitness-For-Service assessment every 5 years to evaluate shell thinning, stress corrosion cracking, and structural fatigue.

3. Escalating Inspection Frequencies

Inspection intervals must automatically tighten as a tank ages, shifting from baseline tracking to aggressive preventative testing.

Tank Age	Internal Inspection Frequency	External Inspection Frequency	Mandatory Testing Scope
0 – 15 Years	Every 10 Years	Every 2 Years	Visual inspection, basic ultrasonic thickness (UT) spot checks.
16 – 30 Years	Every 5 Years	Annually	Full-floor UT scanning, weld seam magnetic particle testing.
31+ Years	Every 3 Years	Semi-annually	Advanced non-destructive testing (NDT), radiography of high-stress joints.

4. Critical Environment Controls (Cooling & Stabilization)

For volatile chemicals prone to runaway polymerization or thermal degradation, cooling systems must be regulated as essential and necessary safety systems.

• Redundant Cooling Loops: Facilities storing chemicals with critical runaway temperatures must utilize dual-independent cooling loops. If the primary refrigeration loop fails, a secondary, mechanically isolated backup loop must activate automatically.
• Emergency Inhibitor Injection: Tanks holding self-reacting monomers must feature an automated, gravity-fed inhibitor injection system. This system must be capable of flooding the tank with stabilizing chemicals within 15 minutes of a runaway heat spike, operating independently of municipal power or manual valves.
• Uninterruptible Power (UPS): Cooling systems, internal temperature probes, and pressure sensors must be hardwired to an on-site, fail-safe backup generator capable of running isolated for a minimum of 72 hours.

5. Vapor Space Management (Moisture & Oxygen Control)

Chemicals that react violently with ambient moisture or require specific oxygen levels to remain stable require active blanket gas regulation.

• Automated Nitrogen Blanketing: For water-reactive or highly flammable chemicals, a positive-pressure nitrogen (or inert gas) blanket system must be mandatory to displace oxygen and humidity.
• Controlled Oxygenation: Some chemicals, like MMA, actually require a precise, low level of dissolved oxygen (typically 20–50 ppm) to keep their stabilizing inhibitors active. Regulations must mandate continuous oxygen-sparging monitoring systems with automated alarms if oxygen levels dip below safe stabilization thresholds.
• Dual-Stage Desiccant Breathers: Any atmospheric venting lines must be equipped with redundant, color-indicating desiccant air breathers to strip 100% of moisture from incoming air during tank drawdown.

6. Valve and Piping Mechanical Integrity

To prevent responders from being locked out during a crisis, mechanical isolation points must be explicitly regulated.

• Quarterly Exercise Mandate: All critical emergency isolation, drainage, and dump valves must be mechanically cycled (exercised) every 90 days to ensure they do not seize or gum up from chemical residue. Logs must be digitally submitted to regulators.
• Fail-Safe Fire Valves: All bottom-outlet lines must feature fire-safe, API 607 certified emergency shutdown valves (ESVs) that automatically close via spring-return mechanisms if external ambient temperatures spike due to a fire.

We no longer live in the 1970’s and are perfectly capable of building and maintaining equipment that meets these standards. Do it.

Private Wells

 

Over the weekend I had a little fun with AI and made up some slides using the EPA website as source material. 

The Case for Funding and Building a Groundwater Monitoring Network

Groundwater is a critical part of our water supply and the hidden reserve that sustains streams, wetlands, private wells, and public water systems during dry periods. In a watershed like the Culpeper Basin, long-term water security depends on keeping withdrawals in balance with recharge. That balance can no longer be assumed. Development has increased impervious cover, droughts have become more consequential, and local observations suggest that groundwater conditions may be changing faster than rainfall alone would explain. Yet we still lack the one thing needed to manage the resource responsibly: a reliable, long-term network of monitoring wells.

Here in Haymarket, there are visible warning signs that deserve attention. Observations from the Bull Run Mountain Conservancy showed perennial streams such as Little Bull Run and Catlett’s Branch going dry during a dry August, while Catharpin Creek was reduced to isolated pools. When streams that are expected to flow year-round begin to fail, that suggests a loss of groundwater support to surface water. In other words, what appears to be a streamflow problem may actually be a groundwater storage problem. Those field observations do not prove the full extent of the issue, but they underscore why direct groundwater monitoring is urgently needed.

Nearby jurisdictions are already building the technical case for systematic monitoring. The Fauquier County Groundwater Resource Assessment and Monitoring Study states that regional- and local-scale data are needed to manage aquifer withdrawals, evaluate water-level declines, identify contributing areas to wells, assess interconnections among pumping wells, and quantify interactions between groundwater and streams. It further notes that surface-water and groundwater monitoring networks are being established specifically to define current conditions and support future investigations. That is directly relevant here: a monitoring network is not simply descriptive; it is the basic infrastructure required to estimate sustainable yield, detect drawdown trends, and evaluate the hydrologic consequences of additional pumping or land use changes.

Regional evidence from Loudoun County points in the same direction. The Assessment of the Groundwater Supply in Loudoun County compiles long-term groundwater, streamflow, and drought information and concludes that groundwater conditions have worsened over the past several decades. The report documents declining water levels, dry wells, springs, and ponds, and argues that parts of western Loudoun are withdrawing groundwater faster than it can be replenished by natural recharge. Whether one accepts every inference in that assessment or not, the central point is difficult to dismiss: without a sufficiently dense and continuous monitoring record, it is impossible to distinguish temporary drought effects from persistent storage decline or to determine whether current withdrawals are within sustainable limits.

That matters because a falling water table affects more than individual wells. As groundwater levels drop, less water remains stored in soil, regolith, and fractured bedrock, and streams can lose the groundwater contribution that keeps them flowing between storms. Once that connection weakens, drought impacts intensify: wells become more vulnerable, streamflow becomes flashier and less reliable, and ecosystems lose the steady baseflow they depend on.

Field observations before and after major land-use change point to a consistent pattern of groundwater stress:

• Wells are being drilled deeper.
• Surface runoff has increased.
• Infiltration and groundwater recharge have decreased.
•  Some ponds, wells, and springs have permanently gone dry.
• The water table has dropped from above the top of bedrock to below it in many locations.
•  Groundwater storage in weathered bedrock has diminished.
•  Some streams and creeks are no longer reliably gaining flow from groundwater and may lose water when nearby wells are pumped.

The cost of waiting can be enormous. When communities discover groundwater problems only after wells fail, the response often shifts from planning to crisis management: emergency well drilling, interconnections, treatment upgrades, or costly new supply projects. A monitoring network is far less expensive than reacting after shortages become acute. It provides the early warning needed to avoid missteps, target conservation measures, and make infrastructure decisions before a water emergency forces them.

This is why proactive planning matters. A groundwater monitoring network would allow local officials, utilities, planners, and residents to track long-term trends, distinguish drought effects from over-withdrawal, identify vulnerable areas, and evaluate whether current land-use and water-supply decisions are sustainable. Without that information, policy is forced to rely on assumptions and guesses. With monitoring, decisions can be based on evidence that is collected over time.

The stakes extend beyond individual wells. The Occoquan Reservoir is one of two major water sources for the Fairfax Water that it supplies water to about one million people in Northern Virginia. Because groundwater storage influences baseflow to tributaries across the watershed, and baseflow in turn contributes to reservoir inflows during dry periods, uncertainty about groundwater conditions is also uncertainty about regional drought resilience. A local monitoring network would therefore support not only private-well protection, but also broader watershed-scale planning around water quantity and hydrologic reliability.

Modeling can be useful, but in fractured-rock aquifers it is inherently a simplification of a highly heterogeneous system. In Virginia’s Piedmont, Blue Ridge, and Mesozoic basin settings, groundwater occurrence and movement vary significantly with local geology, fracture density, weathered-regolith thickness, and topographic position. The Groundwater Characterization and Monitoring Program notes that, in these hard-rock provinces, groundwater occurs mainly in fractures and joints and that hydrogeologic conditions vary substantially from place to place. For that reason, recharge estimates derived from gridded inputs alone cannot establish whether a particular area is recovering seasonally, trending downward over multiple years, or losing hydraulic support to nearby streams. Continuous groundwater-level monitoring is what converts a conceptual understanding of recharge into an observable record of aquifer response.

Soil-Water-Balance (SWB) models often a cheap and quick way to estimate potential recharge, are not direct proof of sustainable yield. The U.S. Geological Survey’s Soil-Water-Balance software is explicitly designed to estimate potential groundwater recharge from daily climate, land use, soil, and flow-direction inputs. The Fauquier County SWB application used that framework to estimate recharge to fractured-rock aquifers and calibrated results in part with base-flow estimates from stream gages. Those are useful screening tools, but they do not directly measure aquifer storage change, drawdown, or the timing and location of recharge transmission through discrete fracture networks. In fractured-rock systems like the Culpeper Basin, water moving below the root zone may still be delayed, diverted laterally, taken up again, or discharged to surface water before it produces measurable recovery in the deeper aquifer tapped by wells. The practical implication is straightforward: modeled recharge can inform hypotheses, but only direct groundwater-level observations can test whether the aquifer is actually recovering at a rate consistent with current and projected withdrawals.

That is the core reason to fund and build a monitoring network now. A well-designed network would provide continuous water-level data, establish local trends, improve drought response, strengthen land-use planning, and help protect both private wells and downstream surface waters. It would also give the public and decision-makers a shared factual basis for difficult choices about growth, conservation, and infrastructure. If groundwater is to remain sustainable, the first step is to measure the system directly and manage it before avoidable damage becomes irreversible.