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Marcellus Shale in Our Community:
    What’s in it for All of Us?


Joint Landowner Coalition of NY Inc.
         February 25, 2011
Source MIT Study of the Future of Natural
Energy Today: New York State Energy
      Consumption Pattern, 2008


37.4%



30.0%



6.0%

24.6%

Σ 98%!
Shale has always been the
hydrocarbon source rock

New technologies make shale
a viable drilling target for
natural gas.

Tightening North American
supply is making
“unconventional resources”
more attractive.

The Barnett showed us that
shale can be exploited.

Numerous domestic shale
opportunities exist
Where Can We Get the Natural Gas ?
  Unconventional Resource Plays




                                  How Much
                               Lewis & Mancos: 97 Tcf
                               New Albany: 86-160 Tcf
                               Barnett: 25-252 Tcf
                               Antrim: 35-76 Tcf
                               Upper Devonian: 225-248 Tcf




                                                             5
Source: NYSERDA
New York Stratigraphy


                     The popular shale




                    Herkimer Sandstone


                    Oneida Sandstone

                   New York’s other shale
Marcellus Structure Contour Map
Unconventional Gas Accumulation




                                  Source-USGS
        Occurs over lager areas
Characteristics of unconventional gas
                shales
 Usually the source rock for other reservoirs
 Organic rich
 Less permeable
 Nuisance gas shows while drilling through the
 formation
 Unusual pressure regimes
 Produced over larger areas
 produce natural gas by stimulation -Hydrofracturing
 Economically produced by using horizontal drilling
 technology
TOC (Total Organic Content)
                           Rock Sample
                                                             Dispersed
                                TOC
                                                              Organic
                                                              Matter:
                                                           the “source”
                                                                 of
                                                         oil + assoc. gas




                   Total Organic Carbon (T.O.C.)

             Live Carbon                       Dead Carbon

      Oil    Organic Matter (Kerogen)              Dead Carbon
Gas               (Jarvie, 1991)
                                        Rock-Eval Terminology
Utica SEM




Porosity is very small and the void are not well connected
Oneida thin section




Porosity here is about 10% and the voids are connected
Regional cross section
The Devonian Marcellus Shale




                                                           (Rickard, 1989)

Primarily interested in Union Springs and Lowermost Oakta Creek Members
Marcellus Union Springs

Organic rich thinly bedded blackish grey to
black shale with thin silt bands
The member is between the Cherry Valley
and Onondaga limestone
Characterized as a pyritiferous, further east
the Union Springs becomes the Bakoven
member that becomes grayer, less organic
and has few limestone members
Lenses in and out in localities in far Western
New York
Marcellus Union Springs




Union Springs with vertical calcite filled fractures in the Onesquethaw
Creek, Albany County, NY
Marcellus Cherry Valley

Consists of skeletal limestones and
shaly intervals
Westward thinning of the Marcellus
Formation in western and central New
York leads to the condensation and
union of the Cherry Valley limestones
with limestones in the upper part of the
Union Springs
Marcellus Cherry Valley




Cherry Valley dark shaly interval and limestone near Cherry Valley, NY
Marcellus Chittenango Member

• Upper member of the Marcellus Formation in
  Western and central New York
• Becomes Cardiff and Chittenango members in
  Central and Eastern New York
• Is confined in Western New York by Stafford
  and Onondaga limestones
• Further east it is between the Stafford and
  Cherry Valley limestones when it is present
• Dark grey to black organic rich shale
Marcellus Oatka Creek




Oatka Creek shale in Oatka Creek, LeRoy, NY
Marcellus (Cherry Valley Isopach)




       ?




The Cherry Valley Limestone Member also thickens to the east
Marcellus (Union Springs Isopach)




    ?



  The Union Springs Member thickens to southeast
Net Thickness of Organic Rich Section of Marcellus




                             (Piotrowski & Harper, 1979)
Shale is Source, Seal and Lately … Reservoir Rock
                                                                                                              Mihai A. Vasilache, 2010


                                                                                                                                          “More mature samples show well-developed
                                                                                                                                          nanopores concentrated in micron-scale
                                                                                                                                          carbonaceous grains. Large numbers of
                                                                                                                                          subelliptical to rectangular nanopores are
                                                                                                                                          present, and porosities within individual grains
                                                                                                                                          of as much as 20% have been observed.
                                                                                                                                          Shallowly buried, lower thermal maturity
                                                                                                                                          samples, in contrast, show few or no pores
                                                                                                                                          within carbonaceous grains.
                                                                                                                                          These observations are consistent with
                                                                                                                                          decomposition of organic matter during
                                                                                                                                          hydrocarbon maturation being responsible for
                                                                                                                                          the    intragranular   nanopores     found    in
                                                                                                                                          carbonaceous grains of higher maturity
                                                                                                                                          samples. As organic matter (kerogen) is
                                                                                                                                          converted to hydrocarbons, nanopores are
                                                                                                                                          created to contain the liquids and gases. With
                                                                                                                                          continued thermal maturation, pores grow and
                                                                                                                                          may form into networks. The specific thermal
                                                                                                                                          maturity level at which nanopore development
                                                                                                                                          begins has not been determined. However,
                                                                                                                                          current     observations   support     nanopore
                                                                                                                                          formation being tied to the onset of conversion
                                                                                                                                          of kerogen to hydrocarbons.”
Picture and text from Robert M. Reed, Bureau of Economic Geology | John A. and Katherine G. Jackson School of Geosciences, The University of Texas at Austin, Austin, TX | Robert G. Loucks , Bureau of
Economic Geology, The University of Texas at Austin, Austin, TX | Daniel Jarvie , Worldwide Geochemistry, Humble, TX | Stephen C. Ruppel , Bureau of Economic Geology, University of Texas at Austin, Austin, TX
 Picture and text from Robert M. Reed, Bureau of Economic Geology | John A. and Katherine G. Jackson School of Geosciences, The University of Texas at Austin, Austin, TX | Robert G. Loucks , Bureau of
 Economic Geology, The University of Texas at Austin, Austin, TX | Daniel Jarvie , Worldwide Geochemistry, Humble, TX | Stephen C. Ruppel , Bureau of Economic Geology, University of Texas at Austin, Austin, TX
HORIZONTAL DRILLING

Combined with Stimulation by

 HYDRAULIC FRACTURING
HORIZONTAL DRILLING

Multiple Wells from One Drill Pad

   6 to 9+ Wells on One Pad

Long Laterals

   1,000 to 8,000 feet
Innovation: Horizontal Drilling
First horizontal well: 1929
First horizontal shale well: 1988
(Antrim Shale in Michigan)
First NYS horizontal: 1989 (and
hundreds drilled since)
“Today, about 2/3rds of the U.S.
rig count is non-vertical, and
close to 50% of the rig count is
drilling horizontal wells.” (Triepke
2010)
Makes multiwell pads possible
                                            National Energy Board (Canada), A Primer for
                                       Understanding Canadian Shale Gas November 2009
200 - 500’             Fresh water aquifers are
                       generally less than 500 feet
                       deep
                       Every casing string is
 400 - 1,200’
                       cemented to surface by
                       pumping cement down pipe
                       and circulating back up
                       between the outside of pipe
                       and the wellbore
                       More than a million pounds of
                       steel casing in each well
2,000 - 2,500’


 To total depth   Source: Range Resources
 30                                                    30
Drilling Rig

            Fresh Water Aquifers




                                          Vertical depth 5,000 – 9,000 feet
   Deep Below the Freshwater
 Aquifers, protected by multiple
 layers of steel casing cemented
 into the ground, water, sand and
 chemicals are pumped to create
 fractures allowing the natural
 gas within the shales to flow
 into the wellbore and up to the
 surface through the steel casing.

   Multiple zones are stimulated
 to maximize reservoir
 stimulation

   During the Treatment, Micro-
 seismic is assisting in evaluating
 the results

                                                                                                                  Hydraulically created fractures
                  Marcellus Shale
                 (100 – 300 feet thick)
                                                                                             Horizontal lateral length
32                                                                                           3,000 – 5,000 feet
HYDRAULIC FRACTURING

Large Volume Hydraulic Fracturing Treatments

  50,000 to 500,000 gallons per stage

Multiple Stages

  4 to 14 Stages per well
Volume Comparison SRBC
Comparable Water Usage Entire Basin
Water Useage For Shale Development
                                      vs
                            Total Water Withdrawal
                              Appalachian Basin




Courtesy John A. Veil Argonne National Laboratory 2010 DUG East Presentation
HYDRAULIC FRACTURING
    WHAT’S IN THE WATER
Additive        Main                 Purpose               Common Use
 Type        Ingredients
            Polyacrylamide    Reduces friction       Cosmetics; soil
Friction    (non-hazardous)   between fluid and pipe conditioner; some
reducer                                              children’s toys

Anti-                         Eliminates bacteria in   Disinfectant; sterilize
Microbial   Glutaraldehyde    the water that produce   medical and dental
Agent                         corrosive byproducts     equipment and
                                                       surfaces
                                                       Automotive anti-
Scale       Ethylene glycol   Prevents scale           freeze, household
inhibitor                     deposit in the pipe      cleaners, de-icing
                                                       agent
            7.5%              Help dissolve cement Swimming pool
Diluted     Hydrochloric      and minerals and help chemical and cleaner
Acid        Acid
                              initiate fractures                                 39
Complements Atlas Energy DUG East 2010
ECONOMIC IMPACT

Jobs
Landowner Royalties
Lease Bonus Payments
State Income Taxes
Local Property Taxes
It’s Happening in Pennsylvania Marcellus 
         Economic Impact ‐ 2010
                         $3.9 billion in total 
                         value added 2009, 
                         $8 billion 2010
                         $389 million in state 
                         and local taxes in 
                         2009, $785 million 
                         2010
                         New jobs 
What About Broome County, NY?
               Let’s Project:
Let’s use the 3 counties       Use NY’s current ad‐
closest to NY in PA: Tioga,    valorem tax structure
Bradford & Susquehanna
                               Use NYSORPS 2010 UOP 
117 wells with over 100        value ($10.14/mcf)
days production reported 
                               Value actual sales at 
to PADEP
                               current gas prices 
Weighted average daily         ($4.77/mcf)
production rate of 3,543 
                               For Detail Utilize Tax 
mcfd
                               allocation from Property 
Assume 1 well is drilled       Tax Bill Town of Maine
NY Real Property Taxes Gas Production
Projection for Marcellus Drilling (1 Well, Town of Maine, Broome Co.)

Avg Well Prod.       3,543              Mcfd
Annual Prod Total    1,293,195          Mcf
NYS UOP Value        $10.14             Per Mcf
Uniform %            70%
                     Taxable Value      Tax Rate/m$   Tax
NYS & Fed Mandate    $9,179,098         11.410278     $104,736
Other County Taxes   $9,179,098         0.000001      $0
Town General         $9,179,098         0.749814      $6,883
Town Highway         $9,179,098         2.762604      $25,358
Maine Fire           $9,179,098         1.932882      $17,742
School Tax           $9,179,098         37.398362     $343,283
Totals                                  54.253941     $498,002
Key Points
1 Well on Town Property In 
        Binghamton
  $498,002 1st yr Local Property Taxes
  $771,613 1st yr Royalty Payments
  $1,269,619 Annual Payments to Town
New York’s Regulatory Environment

 Oil and Gas Drilling and Development has
 been Regulated by the NYS Department of
 Environmental Conservation Division of
 Mineral Resources since its Inception
 around 1969
Welcome to New York Regulation
   State Environmental Quality Review Act
Government agency must review the
environmental impact of its actions.
    Issuance of a permit to drill (and frac)
    a natural gas well is an action which       Generic Environmental 
    requires review.
                                               Impact Statement: 
Disclose and address the impacts that can
be reasonably anticipated.                     Evaluates separate 
Avoid or minimize adverse environmental        actions having common 
impacts to the maximum extent                  impacts
practicable.
The purpose of a SEQRA review is not to
ban an activity, but to identify potential
adverse impacts and ways to mitigate
them.
New York Regulation
  Review & Guidance
1992 GEIS 12 yr effort 4 Volume 937 page 
document (review and study 1980‐1992 
including public hearings across state) 
Supplemental GEIS 800+pages, 9 chapters, 
26 appendices, 114 refs cited by DEC staff, 473 
references cited by NYSERDA consultants 
(included public hearings)
Currrent additional documentation said to be 
more than 1,000 pages reviewing and 
commenting on responses to SGEIS hearings.
Potential Impacts not Addressed by
               GEIS
High-volume fluid management
  Water withdrawals and consumption
  Transportation of water to the site
  Additives
  On-site facilities and handling
  Flowback and ultimate disposition
Multiple wells at single site, longer
duration of impacts
Status of Hydraulic Fracturing in New York
                       Water use                   Permitting status

Horizontal drilling,   GEIS-consistent               Permitted under existing GEIS
no HVHF                                              First horizontal well drilled in 1989
                                                     Horizontal/directional wells
                                                   average 10% of permits per year
                                                     No “moratorium”
Conventional frac      Up to 80,000 gallons/well      Permitted under existing GEIS
(90% of wells in NY;                               finding of no significant impact
552 total permits                                     Disclosure to DEC of water
issued in 2009)                                    source/disposal and frac chemicals
                                                   required with application to drill
High-volume frac       Currently defined as          58 applications pending
(HVHF)                 > 80,000 gallons/well       completion of SGEIS

                       Activity described in
                       dSGEIS: 2 – 8 million
                       gallons
2009 dSGEIS – Disclosures and Mitigation (1)

Concern or      2009 dSGEIS
potential
impact
Water           Impacts of low-flow described; pass-by flow methodology proposed
withdrawals

Spills          Recognizes enhanced risks relative to high-volume hydraulic fracturing
                (i.e., larger volume of chemical additives, larger volume of flowback
                water. Describes NYS spill reporting requirements.
                Enhanced mitigation: Setbacks, secondary containment,
                stormwater permit coverage (SWPPP, BMP’s), review of site-
                layout and fluid disposal plan prior to permit issuance


Wastewater      Reiterates existing procedures and requirements for permitted
disposal        discharges
                Enhanced mitigation: Review and verification of fluid disposal
                plan prior to permit issuance; wastewater tracking to be
                implemented
2009 dSGEIS – Disclosures and Mitigation (2)
Concern or       2009 dSGEIS
potential
impact
Ground water     From surface activities: See spills.
contamination,   From reserve pits & centralized flowback impoundments
including        Enhanced mitigation: Construction and liner specifications/fluid removal
natural gas in   requirements for reserve pits; double liners/leak detection/site-specific
                 engineering review for centralized flowback impoundments
water wells


                 From wellbore: Reiterates existing casing and cementing practices, including annular
                 venting
                 Enhanced mitigation: Cement to surface required on production or intermediate
                 casing; cement bond log; pre-frac certification of wellbore construction




                 From hydraulic fracturing in target zone: Not a reasonably anticipated impact below 2,000
                 feet or with 1,000 feet of vertical separation between target zone and deepest fresh water
                 Enhanced mitigation: Site-specific review at shallower depths or with less vertical
                 separation



                 Baseline testing and ongoing monitoring of nearby water wells
2009 dSGEIS – Disclosures and Mitigation (3)
Concern or           2009 dSGEIS
potential impact

Chemical             dSGEIS lists 197 proposed additives for HVHF
disclosure             6 service companies, 12 chemical suppliers
                       152 with complete compositional information
                       260 unique chemicals with CAS #’s disclosed in dSGEIS: includes amides, amines,
                     petroleum distillates, aromatic hydrocarbons, alcohols, glycol ethers, ethoxylated alcohols,
                     microbiocides, organic acids and related chemicals, polymers, minerals, metals and other
                     inorganics and miscellaneous other chemicals
                     DEC is monitoring developments in other states and at the federal level.



Air quality          Potential well pad impacts: PM, NO2, H2S, benzene
                     Potential off-site compressor impacts: Benzene, NO2, formaldehyde
                     Mitigation: control technologies (fuel, equipment), stack heights, public access
                     restrictions

                     Centralized flowback impoundments: Potential HAP emissions
                     Mitigation options: Eliminate specific compounds (methanol, heavy naptha,
                     benzene), limit duration and use, cover or use tanks instead, physical barriers to
                     public access
                     Will be subject to site-specific review including frac & flowback composition
“Industrialization   Includes descriptions of well pad & equipment size, longer duration of impacts at multi-well
” (noise, visual,    pads; truck traffic associated with HVHF
traffic,             Mitigation: Visual impacts mitigation plan, noise impacts mitigation plan, road
                     use agreement or trucking plan, review of local planning documents, careful
community            access road siting
impacts)             DEC is reviewing many comments on this topic.
THANK YOU

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Marcellus Shale in Our Community: What's in it for All of Us?

  • 1. Marcellus Shale in Our Community: What’s in it for All of Us? Joint Landowner Coalition of NY Inc. February 25, 2011
  • 2. Source MIT Study of the Future of Natural
  • 3. Energy Today: New York State Energy Consumption Pattern, 2008 37.4% 30.0% 6.0% 24.6% Σ 98%!
  • 4. Shale has always been the hydrocarbon source rock New technologies make shale a viable drilling target for natural gas. Tightening North American supply is making “unconventional resources” more attractive. The Barnett showed us that shale can be exploited. Numerous domestic shale opportunities exist
  • 5. Where Can We Get the Natural Gas ? Unconventional Resource Plays How Much Lewis & Mancos: 97 Tcf New Albany: 86-160 Tcf Barnett: 25-252 Tcf Antrim: 35-76 Tcf Upper Devonian: 225-248 Tcf 5
  • 7. New York Stratigraphy The popular shale Herkimer Sandstone Oneida Sandstone New York’s other shale
  • 9. Unconventional Gas Accumulation Source-USGS Occurs over lager areas
  • 10. Characteristics of unconventional gas shales Usually the source rock for other reservoirs Organic rich Less permeable Nuisance gas shows while drilling through the formation Unusual pressure regimes Produced over larger areas produce natural gas by stimulation -Hydrofracturing Economically produced by using horizontal drilling technology
  • 11. TOC (Total Organic Content) Rock Sample Dispersed TOC Organic Matter: the “source” of oil + assoc. gas Total Organic Carbon (T.O.C.) Live Carbon Dead Carbon Oil Organic Matter (Kerogen) Dead Carbon Gas (Jarvie, 1991) Rock-Eval Terminology
  • 12. Utica SEM Porosity is very small and the void are not well connected
  • 13. Oneida thin section Porosity here is about 10% and the voids are connected
  • 15. The Devonian Marcellus Shale (Rickard, 1989) Primarily interested in Union Springs and Lowermost Oakta Creek Members
  • 16. Marcellus Union Springs Organic rich thinly bedded blackish grey to black shale with thin silt bands The member is between the Cherry Valley and Onondaga limestone Characterized as a pyritiferous, further east the Union Springs becomes the Bakoven member that becomes grayer, less organic and has few limestone members Lenses in and out in localities in far Western New York
  • 17. Marcellus Union Springs Union Springs with vertical calcite filled fractures in the Onesquethaw Creek, Albany County, NY
  • 18. Marcellus Cherry Valley Consists of skeletal limestones and shaly intervals Westward thinning of the Marcellus Formation in western and central New York leads to the condensation and union of the Cherry Valley limestones with limestones in the upper part of the Union Springs
  • 19. Marcellus Cherry Valley Cherry Valley dark shaly interval and limestone near Cherry Valley, NY
  • 20. Marcellus Chittenango Member • Upper member of the Marcellus Formation in Western and central New York • Becomes Cardiff and Chittenango members in Central and Eastern New York • Is confined in Western New York by Stafford and Onondaga limestones • Further east it is between the Stafford and Cherry Valley limestones when it is present • Dark grey to black organic rich shale
  • 21. Marcellus Oatka Creek Oatka Creek shale in Oatka Creek, LeRoy, NY
  • 22. Marcellus (Cherry Valley Isopach) ? The Cherry Valley Limestone Member also thickens to the east
  • 23. Marcellus (Union Springs Isopach) ? The Union Springs Member thickens to southeast
  • 24. Net Thickness of Organic Rich Section of Marcellus (Piotrowski & Harper, 1979)
  • 25. Shale is Source, Seal and Lately … Reservoir Rock Mihai A. Vasilache, 2010 “More mature samples show well-developed nanopores concentrated in micron-scale carbonaceous grains. Large numbers of subelliptical to rectangular nanopores are present, and porosities within individual grains of as much as 20% have been observed. Shallowly buried, lower thermal maturity samples, in contrast, show few or no pores within carbonaceous grains. These observations are consistent with decomposition of organic matter during hydrocarbon maturation being responsible for the intragranular nanopores found in carbonaceous grains of higher maturity samples. As organic matter (kerogen) is converted to hydrocarbons, nanopores are created to contain the liquids and gases. With continued thermal maturation, pores grow and may form into networks. The specific thermal maturity level at which nanopore development begins has not been determined. However, current observations support nanopore formation being tied to the onset of conversion of kerogen to hydrocarbons.” Picture and text from Robert M. Reed, Bureau of Economic Geology | John A. and Katherine G. Jackson School of Geosciences, The University of Texas at Austin, Austin, TX | Robert G. Loucks , Bureau of Economic Geology, The University of Texas at Austin, Austin, TX | Daniel Jarvie , Worldwide Geochemistry, Humble, TX | Stephen C. Ruppel , Bureau of Economic Geology, University of Texas at Austin, Austin, TX Picture and text from Robert M. Reed, Bureau of Economic Geology | John A. and Katherine G. Jackson School of Geosciences, The University of Texas at Austin, Austin, TX | Robert G. Loucks , Bureau of Economic Geology, The University of Texas at Austin, Austin, TX | Daniel Jarvie , Worldwide Geochemistry, Humble, TX | Stephen C. Ruppel , Bureau of Economic Geology, University of Texas at Austin, Austin, TX
  • 26. HORIZONTAL DRILLING Combined with Stimulation by HYDRAULIC FRACTURING
  • 27. HORIZONTAL DRILLING Multiple Wells from One Drill Pad 6 to 9+ Wells on One Pad Long Laterals 1,000 to 8,000 feet
  • 28. Innovation: Horizontal Drilling First horizontal well: 1929 First horizontal shale well: 1988 (Antrim Shale in Michigan) First NYS horizontal: 1989 (and hundreds drilled since) “Today, about 2/3rds of the U.S. rig count is non-vertical, and close to 50% of the rig count is drilling horizontal wells.” (Triepke 2010) Makes multiwell pads possible National Energy Board (Canada), A Primer for Understanding Canadian Shale Gas November 2009
  • 29.
  • 30. 200 - 500’ Fresh water aquifers are generally less than 500 feet deep Every casing string is 400 - 1,200’ cemented to surface by pumping cement down pipe and circulating back up between the outside of pipe and the wellbore More than a million pounds of steel casing in each well 2,000 - 2,500’ To total depth Source: Range Resources 30 30
  • 31.
  • 32. Drilling Rig Fresh Water Aquifers Vertical depth 5,000 – 9,000 feet Deep Below the Freshwater Aquifers, protected by multiple layers of steel casing cemented into the ground, water, sand and chemicals are pumped to create fractures allowing the natural gas within the shales to flow into the wellbore and up to the surface through the steel casing. Multiple zones are stimulated to maximize reservoir stimulation During the Treatment, Micro- seismic is assisting in evaluating the results Hydraulically created fractures Marcellus Shale (100 – 300 feet thick) Horizontal lateral length 32 3,000 – 5,000 feet
  • 33. HYDRAULIC FRACTURING Large Volume Hydraulic Fracturing Treatments 50,000 to 500,000 gallons per stage Multiple Stages 4 to 14 Stages per well
  • 34.
  • 36. Comparable Water Usage Entire Basin
  • 37. Water Useage For Shale Development vs Total Water Withdrawal Appalachian Basin Courtesy John A. Veil Argonne National Laboratory 2010 DUG East Presentation
  • 38. HYDRAULIC FRACTURING WHAT’S IN THE WATER
  • 39. Additive Main Purpose Common Use Type Ingredients Polyacrylamide Reduces friction Cosmetics; soil Friction (non-hazardous) between fluid and pipe conditioner; some reducer children’s toys Anti- Eliminates bacteria in Disinfectant; sterilize Microbial Glutaraldehyde the water that produce medical and dental Agent corrosive byproducts equipment and surfaces Automotive anti- Scale Ethylene glycol Prevents scale freeze, household inhibitor deposit in the pipe cleaners, de-icing agent 7.5% Help dissolve cement Swimming pool Diluted Hydrochloric and minerals and help chemical and cleaner Acid Acid initiate fractures 39
  • 40. Complements Atlas Energy DUG East 2010
  • 41.
  • 42. ECONOMIC IMPACT Jobs Landowner Royalties Lease Bonus Payments State Income Taxes Local Property Taxes
  • 43.
  • 44. It’s Happening in Pennsylvania Marcellus  Economic Impact ‐ 2010 $3.9 billion in total  value added 2009,  $8 billion 2010 $389 million in state  and local taxes in  2009, $785 million  2010 New jobs 
  • 45. What About Broome County, NY? Let’s Project: Let’s use the 3 counties  Use NY’s current ad‐ closest to NY in PA: Tioga,  valorem tax structure Bradford & Susquehanna Use NYSORPS 2010 UOP  117 wells with over 100  value ($10.14/mcf) days production reported  Value actual sales at  to PADEP current gas prices  Weighted average daily  ($4.77/mcf) production rate of 3,543  For Detail Utilize Tax  mcfd allocation from Property  Assume 1 well is drilled Tax Bill Town of Maine
  • 46.
  • 47. NY Real Property Taxes Gas Production Projection for Marcellus Drilling (1 Well, Town of Maine, Broome Co.) Avg Well Prod. 3,543 Mcfd Annual Prod Total 1,293,195 Mcf NYS UOP Value $10.14 Per Mcf Uniform % 70% Taxable Value Tax Rate/m$ Tax NYS & Fed Mandate $9,179,098 11.410278 $104,736 Other County Taxes $9,179,098 0.000001 $0 Town General $9,179,098 0.749814 $6,883 Town Highway $9,179,098 2.762604 $25,358 Maine Fire $9,179,098 1.932882 $17,742 School Tax $9,179,098 37.398362 $343,283 Totals 54.253941 $498,002
  • 48. Key Points 1 Well on Town Property In  Binghamton $498,002 1st yr Local Property Taxes $771,613 1st yr Royalty Payments $1,269,619 Annual Payments to Town
  • 49. New York’s Regulatory Environment Oil and Gas Drilling and Development has been Regulated by the NYS Department of Environmental Conservation Division of Mineral Resources since its Inception around 1969
  • 50. Welcome to New York Regulation State Environmental Quality Review Act Government agency must review the environmental impact of its actions. Issuance of a permit to drill (and frac) a natural gas well is an action which Generic Environmental  requires review. Impact Statement:  Disclose and address the impacts that can be reasonably anticipated. Evaluates separate  Avoid or minimize adverse environmental actions having common  impacts to the maximum extent impacts practicable. The purpose of a SEQRA review is not to ban an activity, but to identify potential adverse impacts and ways to mitigate them.
  • 52. Potential Impacts not Addressed by GEIS High-volume fluid management Water withdrawals and consumption Transportation of water to the site Additives On-site facilities and handling Flowback and ultimate disposition Multiple wells at single site, longer duration of impacts
  • 53. Status of Hydraulic Fracturing in New York Water use Permitting status Horizontal drilling, GEIS-consistent Permitted under existing GEIS no HVHF First horizontal well drilled in 1989 Horizontal/directional wells average 10% of permits per year No “moratorium” Conventional frac Up to 80,000 gallons/well Permitted under existing GEIS (90% of wells in NY; finding of no significant impact 552 total permits Disclosure to DEC of water issued in 2009) source/disposal and frac chemicals required with application to drill High-volume frac Currently defined as 58 applications pending (HVHF) > 80,000 gallons/well completion of SGEIS Activity described in dSGEIS: 2 – 8 million gallons
  • 54. 2009 dSGEIS – Disclosures and Mitigation (1) Concern or 2009 dSGEIS potential impact Water Impacts of low-flow described; pass-by flow methodology proposed withdrawals Spills Recognizes enhanced risks relative to high-volume hydraulic fracturing (i.e., larger volume of chemical additives, larger volume of flowback water. Describes NYS spill reporting requirements. Enhanced mitigation: Setbacks, secondary containment, stormwater permit coverage (SWPPP, BMP’s), review of site- layout and fluid disposal plan prior to permit issuance Wastewater Reiterates existing procedures and requirements for permitted disposal discharges Enhanced mitigation: Review and verification of fluid disposal plan prior to permit issuance; wastewater tracking to be implemented
  • 55. 2009 dSGEIS – Disclosures and Mitigation (2) Concern or 2009 dSGEIS potential impact Ground water From surface activities: See spills. contamination, From reserve pits & centralized flowback impoundments including Enhanced mitigation: Construction and liner specifications/fluid removal natural gas in requirements for reserve pits; double liners/leak detection/site-specific engineering review for centralized flowback impoundments water wells From wellbore: Reiterates existing casing and cementing practices, including annular venting Enhanced mitigation: Cement to surface required on production or intermediate casing; cement bond log; pre-frac certification of wellbore construction From hydraulic fracturing in target zone: Not a reasonably anticipated impact below 2,000 feet or with 1,000 feet of vertical separation between target zone and deepest fresh water Enhanced mitigation: Site-specific review at shallower depths or with less vertical separation Baseline testing and ongoing monitoring of nearby water wells
  • 56. 2009 dSGEIS – Disclosures and Mitigation (3) Concern or 2009 dSGEIS potential impact Chemical dSGEIS lists 197 proposed additives for HVHF disclosure 6 service companies, 12 chemical suppliers 152 with complete compositional information 260 unique chemicals with CAS #’s disclosed in dSGEIS: includes amides, amines, petroleum distillates, aromatic hydrocarbons, alcohols, glycol ethers, ethoxylated alcohols, microbiocides, organic acids and related chemicals, polymers, minerals, metals and other inorganics and miscellaneous other chemicals DEC is monitoring developments in other states and at the federal level. Air quality Potential well pad impacts: PM, NO2, H2S, benzene Potential off-site compressor impacts: Benzene, NO2, formaldehyde Mitigation: control technologies (fuel, equipment), stack heights, public access restrictions Centralized flowback impoundments: Potential HAP emissions Mitigation options: Eliminate specific compounds (methanol, heavy naptha, benzene), limit duration and use, cover or use tanks instead, physical barriers to public access Will be subject to site-specific review including frac & flowback composition “Industrialization Includes descriptions of well pad & equipment size, longer duration of impacts at multi-well ” (noise, visual, pads; truck traffic associated with HVHF traffic, Mitigation: Visual impacts mitigation plan, noise impacts mitigation plan, road use agreement or trucking plan, review of local planning documents, careful community access road siting impacts) DEC is reviewing many comments on this topic.