Custom Search
MARCELLUS
SITE MAP
Home
Terms of use
Contact us
Links
Resources
Search site
DRILLING NEWS
Jobs
Blogs
News-Events
New pages
Now drilling
LEGISLATION
Drilling legislation
Engaged citizens
The FRAC Act
Halliburton loophole
Political Contributions
DRILLING ISSUES
Intro to Marcellus
Air quality
Before you lease
Lessons learned
Talking points
ALL HAIL Marcellus Shale
WATER ISSUES
WANTED: Water
Brine truck photos
Clairton Municipal Authority
Creeks & waterways
Drilling wastewater
Dunkard Creek
Impoundments
McKeesport Municipal Authority
Monongahela River
Pets & gas drilling wastewater
Piping water
Seeps, leaks, spills
MARCELLUS PLAY
Best Production Pad
Cross Creek Park
Diesel idling - Act 124
Frac truck photos
Gas facilities
Gas flares
Gas pipelines
Gas shale plays
Gas well fires
Hoskins Unit
Kearns Unit
Marcellus FRAC
Photos of gas wells
Restored well sites
Road damage
Rodenski Unit
Trinity South
Truck traffic
YouTube Marcellus
THE PLAYERS
Advanced Waste Services
Allan's Wastewater
Anadarko
Arrow Energy
Atlas Energy
Baker Tanks
Baker-Hughes
Bobcat Pressure Control
Bronco Oilfield Services
Buckeye Partners
Cabot Oil & Gas
Carrizo Oil & Gas
Chesapeake Energy
Chief Oil & Gas
C.J. Hughes
CNX Gas
Columbia Gas Transmission
Dawson Geophysical
Devonian Industries
Dominion
East Resources
Eastern American Energy Corp.
Eastern Reservoir Services
EnCana
Energy Contractors
EOG Resources
Ergon Trucking
EQT
EXCO Resources
Fortuna Energy
Frac Tech
Great Lakes Energy Partners
Halliburton
Hawg Hauling
Laurel Mountain Midstream
Liquid Assets Disposal
MarkWest
MicroSeismic
Multi-Chem
National Fuel
National Oilwell Varco
Patterson Drilling
Penneco
Pennsylvania Brine Treatment
Pennsylvania DEP
Pennsylvania General Electric
PostRock/Quest
Range Resources
Red Oak Water Transfer
Rex Energy
Rice Energy
Schlumberger
Seneca Resources
Southwestern Energy
Spectra Energy
Stallion Construction
Stone Energy
Strata Directional Technology
Superior Well Services
SW Jack Drilling Co
Ultra Resources
USA Compression
Waste Treatment Corporation
Williams Companies
XTO Energy
 

Our look at the
MONONGAHELA RIVER
or 'MON RIVER'

Since the increase of Marcellus Shale gas drilling in West Virginia and Pennsylvania, one river has felt most of the effects -- the Monongahela River -- which is known to residents simply as "The Mon." As steelmaking and other heavy industries left the banks of the Monongahela River toward the end of the 20th Century, water quality improved enough that Pittsburgh hosted the 2005 BassMaster competition. Things were looking up for The Mon.
  
Then gas drilling, with its hydraulic fracturing process, began early in the 21st Century and began to "tip the balance" of existing river water conditions. This was not only an important development for fish and aquatic life, but also the millions of Pittsburgh area residents who get their tap water from water treatment plants located along the Mon.
  
These conditions first became obvious in late-2008 when water showed over the limit TDS (total dissolved solid) levels. Residents noticed the bad taste and smell of their drinking water, as well as spotted dishes coming out of their dishwashers. Plumbers began noticing black deposits in plumbing fixtures.
  
  

THE MON
The Monongahela River flows 128 miles from Fairmont West Virginia to Pittsburgh Pennsylvania and is one of very few US rivers that flows north. The Native American word 'Mechmenawungihilla' or 'Monongahela' means "falling banks" and refers to its unstable river banks.

  
When high-TDS water is chlorinated it creates trihalomethanes (THM or THMM) which water customers are told is safe to drink. However, one water expert warned of health dangers when these same chemicals in the water "gas off" and get inhaled while someone is taking a hot shower or bath.
  
This high-TDS situation is created by a couple factors:
1) low river flow in the Mon River and
2) the dumping of drilling brine into the Mon
  
Low river flow occurs primarily during drought periods. Fall 2008 was very dry with a Pennsylvania drought warning finally being issued on November 7th. This low water condition was aggravated by drillers taking free water out of local streams and watersheds to provide the millions of gallons of water required to frack (correct spelling is 'frac' which is short for fracture) each Marcellus Shale gas well. There are environmental regulations concerning the 'dewatering' of streams, but enforcement is lax to non-existent in southwestern Pennsylvania.
  
The dumping of drilling brine back into Pittsburgh tap water sources became a serious issue when ill-equipped waste treatment plants were accepting all the drilling wastewater they could get. The extra business improved their bottom lines. However, most were not equipped to handle industrial grade wastewater and much of the processing was incomplete. Even well-equipped treatment plants have difficulty removing salts from water, so they count on dilution as the key to solving a high TDS problem. The more drilling brine is watered-down, the story goes, the closer the water will come to having acceptable quality levels.
  
Pennsylvania finally caught up with the dumping end of this equation, by the DEP limiting how much wastewater facilities could accept, and which ones could accept it. This created some temporary improvements in early 2009, but dry weather conditions in late Spring and early summer began triggering 'over the limit' announcements by various water treatment authorities once again. Some facilities hired consultants to work on their problem, and ended up switching their water purification away from chlorine, to eliminate the trihalomethane situation.
  
So let's take a look at some photos of the Monongahela River as it flows from West Virginia toward Pittsburgh, Pennsylvania.
  

Monongahela River flowing past West Virginia University in Morgantown
  
  
Mon River near where it enters Pennsylvania from West Virginia near Point Marion
  
  
Looking down on the Cheat River from Cooper's Rock
  
  
Cheat River right above the confluence with the Mon River at Point Marion
  
  
Welcome to Point Marion Pennsylvania
Est. 1842
Home of the Albert Gallatin Regatta
  
  
Confluence of the Monongahela River and Cheat River at Point Marion, Pa
  
  
Mon River water below the Two Rivers confluence
  
  
The Monongahela River flows north from Point Marion to Pittsburgh
  
  
"The Mon" flowing past Brownsville Pennsylvania
  
 
Towboat with barges plys the Mon River near Monongahela, Pa
  
  
The Monongahela River by Station Square in Pittsburgh, Pa
  
  
Bridges crossing the Mon near Pittsburgh's South Side
  
  
Polar Bear event in the Monongahela River on New Year's Day
  
  
With Mount Washington and the Fort Pitt Bridge in the background, television news crews interview the organizer of the Polar Bear event
  
  
Looking down the Mon toward its confluence with the Allegheny River at The Point in Pittsburgh, Pennsylvania. The Monongahela River joins the Allegheny River to form the Ohio River, hence the name "Three Rivers Stadium" for the first Steelers/Pirates stadium near the confluence of these three rivers.
  
 

Below is an extract from a Pennsylvania DEP document dated November 7, 2009. It is part of Proposed Rulemaking for Wastewater Treatment Requirements in Pennsylvania, and offers some additional insights into the Mon River problem with high- TDS.
  


PROPOSED RULEMAKING
[25 PA. CODE CH. 95]
Wastewater Treatment Requirements
[39 Pa.B. 6467]

PA Bulletin, Doc. No. 09-2065
http://www.pabulletin.com/secure/data/vol39/39-45/2065.html

[Saturday, November 7, 2009]

The Environmental Quality Board (Board) proposes to amend 25 Pa. Code Chapter 95 (relating to Wastewater Treatment Requirements). The proposed amendments include the elimination of a redundant provision, the recognition of applicable TMDL requirements, and the establishment of new effluent standards for new sources of wastewaters containing high Total Dissolved Solids (TDS) concentrations.

The proposal was adopted by the Board at its meeting of August 18, 2009.

 Code of 1929 (71 P. S. §§ 510-7 and 510-20).

D. Background and Purpose

Total dissolved solids (TDS) is comprised of inorganic salts, organic matter and other dissolved materials in water. They can be naturally present in water or the result of runoff, mining or industrial or municipal treatment of water. TDS contain minerals and organic molecules that provide benefits such as nutrients, but also may contain contaminants such as toxic metals and organic pollutants. However, the benefits noted are when considered in moderation, which is likely not the case in a high TDS discharge. The concentration and composition of TDS in natural waters is determined by the geology of the drainage, atmospheric precipitation and the water balance (evaporation/precipitation).

TDS causes toxicity to water bodies through increases in salinity, changes in the ionic composition of the water, and toxicity of individual ions. The composition of specific ions determines toxicity of elevated TDS in natural waters. Also, as the hardness increases, TDS toxicity may decrease. The major concern associated with high TDS concentrations relates to direct effects of increased salinity on the health of aquatic organisms.

Water quality analyses performed for the major watersheds of this Commonwealth to date, show that many of the rivers and streams of this Commonwealth have a very limited ability to assimilate additional TDS, sulfates and chlorides. This phenomenon was most evident during the fall of 2008, when actual water quality issues related to these parameters emerged in the Monongahela River basin. While river flows reached seasonal lows, the concentrations of TDS and sulfates in the river increased to historic highs, exceeding the water quality standards at all of the 17 Potable Water Supply intakes from the border with West Virginia to Pittsburgh. Exceedances of water quality standards for TDS and sulfate persisted in the river through November and December of 2008. Elevated chloride levels were observed on at least one major tributary—South Fork Tenmile Creek—and for the first time, elevated bromide levels were observed in these streams.

During this period, several environmental agencies performed studies on the effects of TDS, sulfate and chloride discharges on the Monongahela and some of its tributaries. A study conducted by the Environmental Protection Agency (EPA), the Department and the Allegheny County Health Department (ACHD) also identified bromides as a key parameter of concern in these waters. The study concluded that a high percentage of the Disinfection By-Products (DBPs) being formed in the drinking water systems were brominated DBPs, which pose a greater health risk than chlorinated DBPs; and, subsequent formation of brominated DBPs increases overall DBP concentrations, specifically trihalomethanes (THMs). The study also concluded that based on the speciation there appears to be a strong correlation between THM formation and elevated source water bromide concentrations in the Monongahela River. As a result, the 17 potable water supply intakes on the Monongahela River are subject to higher levels of the more toxic brominated DBPs, creating increased risks of bladder cancer to their consumers.

Several studies on the potential impacts to aquatic life from these large TDS discharges were also conducted on major tributaries flowing into the Monongahela River in Greene County, PA. Each of these studies documents the adverse effects of discharges of TDS, sulfates and chlorides on the aquatic communities in these receiving streams. The former concludes that there is a high abundance of halophilic (salt-loving) organisms downstream from the discharges of TDS and chlorides and a clear transition of fresh water organisms to brackish water organisms in the receiving stream from points above the discharge to points below. It is evident from this study that increases in salinity have caused a shift in biotic communities.

The Monongahela River Watershed is being adversely impacted by TDS discharges and many points in the watershed are already impaired, with TDS, sulfates and chlorides as the cause.

Although the Monongahela has received the most attention, it is not an anomalous situation. The Department has studied the results of stream monitoring and has conducted an analysis on the water quality of the Beaver River in western Pennsylvania. These results show upward trends in TDS concentrations. The Department has also conducted similar studies on the Shenango and Neshannock Rivers, with similar upward trends in TDS concentrations.

In addition, watershed analyses conducted by the Department of the West Branch of the Susquehanna River and the Moshannon River Watersheds have documented that they are also severely limited in the capacity to assimilate new loads of TDS and sulfates. The Department has received several permit applications in these areas where the permits will not be able to be issued with limits greater than the water quality standards due to the high background concentrations of TDS.

The surveys, analyses and studies referenced establish that the extent of existing and potential pollution from TDS, sulfates and chlorides is widespread. The Department is constrained from approving any significant portion of the pending proposals and applications for new sources of discharge high-TDS wastewater that include sulfates and chlorides, and still protect the quality of streams in this Commonwealth.

The existing practice for high TDS wastewaters is the removal of heavy metals, but currently no treatment exists for TDS, sulfates and chlorides, other than dilution. As documented by the rising levels of TDS in the waters of this Commonwealth, dilution can no longer be considered adequate treatment for high TDS wastewaters.

The Clean Streams Law (35 P. S. §§ 691.1—691.1001) delegates the authority to preserve and improve the purity of its waters and develop remedies to purify those waters currently polluted to the Department, in the form of adopting rules and regulations as necessary to accomplish these tasks.

The Department's ''Permitting Strategy for High Total Dissolved Solids (TDS) Wastewater Discharges'' (April 11, 2009) outlines the foundation and scientific rationale for promulgation of such rules and regulations necessary to address the existing and potential pollution of this Commonwealth's waters from large sources of TDS, sulfates and chlorides. This approach relies upon the basic water quality management premise that discharges of these pollutants must be managed through permit limitations required by the more stringent of treatment-based or water quality-based standards.

The goal of this permitting strategy is that by January 1, 2011, new sources of High-TDS wastewaters will be prohibited from this Commonwealth's waters. To achieve this goal, the Department proposes to amend Chapter 95 to establish new effluent standards.

In addition to moving this regulatory package forward, the Department is considering, on a parallel track, the formation of a work group in the Monongahela River Watershed to review possible alternative approaches that would also be protective of this Commonwealth's water resources.

The proposed rulemaking was presented to the Water Resources Advisory Committee (WRAC) at a special meeting on June 19, 2009, and considered at the WRAC's regular meeting on July 15, 2009. The WRAC, by majority vote, recommended that the Department work in conjunction with the WRAC to form a Statewide stakeholders group to analyze the issues and develop appropriate solutions, in lieu of proceeding with the currently proposed rulemaking.
  

FULL TEXT: http://www.pabulletin.com/secure/data/vol39/39-45/2065.html
   


LINKS

Monongahela River TDS, Chloride, and Sulfate Sampling Results
(PA DEP - PDF)

Upper Monongahela River Association, Inc.

 

  
  

Hit Counter


home     terms of use     contact     search site
Copyright ©2009-2010    Marcellus-Shale.us    All rights reserved.