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~ecessily taught in the field and 03 a one-on--one basis. A<br />

classroozi discussion of the results and the significance of the<br />

data was givei? to show the relationship between individual well<br />

kasts and the respective geologic areas- Those individuals who<br />

bad the o:p<strong>part</strong>ar;ty to attend the E.S. Geological Suwey short<br />

course an groundwaZer %end to do well an data collection and<br />

interpretation. Adeitional training and axperience is needed by<br />

all Sydxogeoisqists j.n this effort-<br />

There are at tkfs time five hydrageologists, and five<br />

assistant ~ydrogeologists In cou2try with sufficient training to<br />

be of service to the MCh drilling operations. Three<br />

hydrogeologist cse completing their degree programs at the<br />

Gnlvsrsity of Arizona, and are expected to return soon. Several<br />

af these individuals have requested enrollment in a groundwater<br />

corresg~ndencs course offered by Wright State University.<br />

Training of personsel az the ?Whi laboratory faced the same<br />

problems as ail groups. nzmaly, lack of attendance and lack of<br />

incentive to <strong>part</strong>icipate iii training activities. The laboratory<br />

had a staff of twenty-five, Sut only one was a professional<br />

ckezist. The fey who attended on a regular basis had been<br />

previausly trafned in basic analytical work, and were able to<br />

perfom some geochemical analyses under s ~pe~isian, but were<br />

nat able to perform routine water analyses.<br />

W i t h the initiation of the CGDP, five professional chemists<br />

and two l.aboxzt3ry technicians were recrc ited, All. the<br />

pr~fessionai chemists and one laboratory technician have<br />

received, us are receiving, training in the U.S. Tvo of the<br />

cheaists Ire still in the G.S., two have been released, and<br />

three are still ~orXFng zt the laboratory. Those individuals<br />

staying with the progrzm have received 03T for water chemistry,<br />

nicraSi03~gy f ielZ " -s%, water qua2i ky daza interpretati,on and<br />

rarer% writing.<br />

Trior to introducing analytical water analysis techniques,<br />

fcms fur receiving samples and for registering results were<br />

cevelope6. These fam.s have bee2 made a <strong>part</strong> of the established<br />

lzboratory prccedure for wzter analyses. Figures 2.2,l and<br />

2.2.2 tre exomples of these fo,lr..s.<br />

TraFnizg was ~Fve? in " ,he preparation of analytical<br />

routines for water sa~ple analyses after the methods were<br />

standarbired by the consultantst cnemist. Standardization<br />

consisted of developing techniques compatible with the<br />

laboratory epip~ent~ extrexes in water cpafity and available<br />

reagents. Seventeen paraxeters were standardized that included:<br />

EC, T>S, ?if, Ca, Hg, IS, X+, I(, CL, 5D4, HCD NOa, 3, WH4, Fe,<br />

E Z Si.<br />

3<br />

~ 9f these, routire analyses were developed for eleven

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