IN THE BEGINNING THERE WAS SALT J.Q. DICKINSON SALT WORKS 1938 - PowerPoint PPT Presentation

IN THE BEGINNING THERE WAS SALT

J.Q. DICKINSON SALT WORKS 1938 Nuttall Sandstones

AND NOW WE HAVE SALT AGAIN https tps://www.google.com/maps ps/@38. 38.29 29112 1278 78,- 81. 1.562033 620337, 7,3a 3a,75 75y,109. 09.68h 68h,84. 4.85t/ 85t/data ta=! =!3m 3m8! 8!1e 1e1! 1!3m 3m6! 6!1s 1s- pMJAXd XdaZHzI%2FWHgeKnsAFNI%2FAAAAAAAABhE%2Fr0Z6QoL oLOOBoDhX2YKmN NkKsZmHiOvx2V 2VgCL CLIB!2e 2e4! 4!3e 3e11! 1!6s 6s%2F 2F%2F 2Flh5. 5.googleusercontent.co com%2F 2F- pMJAXd XdaZHzI%2FWHgeKnsAFNI%2FAAAAAAAABhE%2Fr0Z6QoL oLOOBoDhX2YKmN NkKsZmHiOvx2V 2VgCL CLIB%2F 2Fw20 203-h10 100-k-no no-pi pi-1.0124 24031 31-ya195. 95.56 56804 804-ro ro- 5.1163 6378 78-fo100% 00%2F 2F!7i 7i53 5376! 6!8i 8i2688 2688

WHICH BEGOT OIL

MORE SPECIFICALLY THE CABIN CREEK OIL FIELD Berea Sandstone

MINE POOLS IN AT LEAST FOR FOUR COAL SEAMS

EAGLE COAL SEAM STRUCTURE

EAGLE SEAM SAMPLING

SO CALLED CHILTON

STOCKTON AND STOCKBURG

SURFACE MINING

GROUND WATER SITES

THE ANALYSIS Cation/ on/Ani nion on  Magnesium and Sulfate  Calcium and Carbonate  Sodium/Potassium and Chloride Tracer E Elements  Barium, Strontium, and Bromide  Selenium

PIPER DIAGRAM Shallow and Elevated Deep Water

DEEP WATERS Very High TDS, Na, K and Cl Very High Barium, Strontium and Bromide Very Low Selenium

DEEP SOURCE MINE POOLS AND JOES CREEK WELLS Progressively Higher TDS, Na, K and Cl with increasing depth. Likewise Barium, Strontium and Bromide

SURFACE MINE AND ELEVATED MINE POOL DOMINATED IMPACTS High Sulfates and elevated Magnesium and Calcium Low Barium, Strontium and Bromide

ELEVATED POOL WITH DEEP WATER INFLUENCE

LOOKING ACROSS JOES CREEK https tps://www.google.com/maps ps/@38. 38.1054 054799, 799,- 81. 1.5443866, 43866,3a 3a,75y 75y,236. 236.25h 25h,89. 89.25t/ 25t/data ta=! =!3m 3m8! 8!1e 1e1! 1!3m 3m6! 6!1s 1s- 1MCDZOBWXYY%2FWOJCjRXl XllTI% I%2FAAAAAAAADF8%2FIv Iv-HmWxs xsRaQgqyN- JzNjOg88k 88kj-SZDdIwCLIB!2e 2e4! 4!3e 3e11! 1!6s 6s%2F 2F%2F 2Flh4. 4.googleusercontent. t.com%2F 2F- 1MCDZOBWXYY%2FWOJCjRXl XllTI% I%2FAAAAAAAADF8%2FIv Iv-HmWxs xsRaQgqyN- JzNjOg88k 88kj-SZDdIwCLIB%2F 2Fw203 203-h100-k-no no-pi pi-0.00203 002033262 3262-ya349. 49.952 95224- ro3.452 4524739 739-fo100% 0%2F 2F!7i 7i53 5376! 6!8i 8i2688 2688

OLD SOURCE SEEPS

SODIUM TO CHLORIDE So Sodiu ium:Chloride R Rat atio io 30 25 25 U-0391 Pump 8 SK1 Joes Creek south bank 20 Little White Oak, Right Fork Seep Little White Oak, Right Fork Upstream 15 Remington Main Portal 10 U-64-83 Chilton Punch Mine, Joes Creek 5 Valley Fill 1.14 0.94 0.88 0.93 0.83 0.81 0.79 0 2013 Brine Ratio 0.69

CHLORIDE TO BROMIDE Chlori ride:Bromide R Ratio 2500 2,276 2000 U-0391 Pump 8 SK1 Joes Creek south bank 1500 Little White Oak, Right Fork Seep Little White Oak, Right Fork Upstream Remington Main Portal 1000 U-64-83 495 Chilton Punch Mine, Joes Creek 448 451 447 385 500 Valley Fill 134 113 0 2013 Brine Ratio 180

BARIUM TO STRONTIUM Barium: m:Str tronti tium R m Ratio 0.2 0.18 0.16 U-0391 Pump 8 SK1 0.14 Joes Creek south bank 0.12 Little White Oak, Right Fork Seep Little White Oak, Right Fork Upstream 0.1 Remington Main Portal 0.08 U-64-83 0.06 Chilton Punch Mine, Joes Creek 0.04 Valley Fill 0.02 0 2013 Brine Ratio 1.47

FINDINGS 1. Gr Groundwater and nd m mine ne po pools show a variety o of d deep a p and nd s shallow g groundwater influen ences es. 2. Cat ation/A /Anion An Anal alysis can an gr great eatly h hel elp s sort shal allow an w and deep eep source e gr ground wat ater. 3. Barium, m, Strontium m and Bromi mide levels h help further er d differ erentiate g ground wa water where shallow a and nd d deep p sour urce m mixing i is o occur urring.

QUESTIONS???