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subaqueous exposure, compared to Type I, and has no anhydrite-gypsum, polyhalite or<br />

mudstone-layers. The cumulative thickness <strong>of</strong> Type II exceeds that <strong>of</strong> Type I in the<br />

McNutt (Lowenstein, 1988).<br />

Other hypotheses on the origin <strong>of</strong> Ochoan rocks near Carlsbad, NM, differ<br />

sughtly to greatly from the classic reflux model. Leslie et al. (1993) believe that the<br />

laminated couplets <strong>of</strong> anhydrite and calcite/organic material, interbedded WIth massive to<br />

poorly laminated halite in the Castile and Salado Formations, were formed below wave<br />

base during a period <strong>of</strong> restricted circulation <strong>of</strong> marine water. Anderson (1993) suggests<br />

that the Castile Formation may be a "nonmarine" evaporite with considerable meteoric<br />

recharge.<br />

MINING<br />

The high solubility <strong>of</strong> most potash ores under New Mexico climates limits them to<br />

the subsurface-hence all mines in the CPD are underground. Mine depths range from<br />

about 270 to 425 m. These room-and-pillar mines ar~ relatively clean, dry, and orderly<br />

because the beds being exploited are relatively shalL' regular, tabular, and nearly flat.<br />

Room-and-pil1ar mining is flexible and allows selective mining (Sullivan and Michael,<br />

1986) so salt horses are easily bypassed and ore grade control is good. The location <strong>of</strong><br />

barren salt horses is unpredictable, but they comprise up to 10% <strong>of</strong> the ore horizons and<br />

must be avoided. Low concentrations <strong>of</strong> methane are rarely encountered. Relief holes are<br />

drilled in ceilings to dissipate nitrogen (Williams-Stroud et ai., in press All mines in the<br />

CPD consist <strong>of</strong> at least two shafts for safety and ventilation and older ,;:mes have three or<br />

more shafts because working f~,;es are now 5-8 km, or more, from the main shaft<br />

(Searls, 1985).<br />

Continuous mining equipment adapted from coal mining is used to mine most<br />

potash ore although blasting is also used. Beds as thin as 1.2 m are mined w,th mechanical<br />

drum miners. Some harder ores, particularly langbeinite, require mecharllcal undercutters<br />

to prepare the working lace for drilling and blasting, usually with Ai'-l"FO (ammonium<br />

nitrate and fuel oil). In all cases, mechanical loaders, underground crushers, and<br />

conveyor belts are used to handle broken ore. Room-and-pillar methods remove 60-75%<br />

<strong>of</strong> the ore during initial mining. Subsequent removal <strong>of</strong> most <strong>of</strong> the support pillars allows<br />

exttaetion to exceed 90% (Sullivan and Michael, 1986; Barker and Austin, 1993). This is<br />

not done routinely, particularly when nnmined overlying ore zones are present, but is<br />

usually done only when an area <strong>of</strong> the mine is being permanently closed.<br />

MILLING<br />

Mills in the CPD produce potash by combinations <strong>of</strong> separation, flotation,<br />

crystallization, leaching, and heavy media circuits related to speciftc ore. Output from<br />

these circuits is dried in fluid bed or rotary dryers and sized over screens to yield fmal<br />

products. Potash ore is ground to break up sylvite-halite agglomerates (Searls, 1985)<br />

<strong>Information</strong> <strong>Only</strong><br />

III-7

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