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A sensitive method was developed for the determination of free morphine and codeine in blood. This method is suitable for detection of the ingestion of illicit drugs. This test is applicable for monitoring therapeutic doses as well as stand up in the court of law. For the test we use with deuterium tagged morphine and codeine. We tag the blood specimens with deuterium prior to testing. The active ingredients (morphine and codeine) are extracted by solid phase extraction, and eventually derivatized with pentafluoro propionic anhydride (PFPA). The resulting compounds are stable and have good chromatographic characteristics. The Gas-chromatograph coupled Mass-spectrometer (GC/MS) system is used to determine the concentration of the resulting compounds using or/in the selective ion mode (SIM). The results of the target and qualifier ions were 414, 577, 361 in the case of morphine, and 282, 445 in the case of codeine. During our measurements, the graph was linear between 1 and 100 ng / mL. All the results of the qualifications were in line with the German Standards DIN 32645, which were checked with the B.E.N. program.

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Agrokémia és Talajtan
Péter Csathó
E. Osztoics
J. Csillag
T. Lengyel
L. Gonda
L. Radimszky
G. Baczó
M. Magyar
K. R. Végh
M. Karátsonyi
T. Takács
A. Lukács
, and
T. Németh

Depending on their origin, sedimentary phosphate rocks (PRs) may differ in their P solubility, and, as a consequence, in their agronomic effectiveness. The effect of six phosphate rocks (PR) - originating from Algeria (ALG), North Florida (FLO), North Carolina (NCA), Senegal (SEN) Morocco (MOR) and Hyperphosphate (HYP) with various P solubility (evaluated by 2% formic acid, 2% citric acid, and neutral ammonium citrate) - as well as single superphosphate (SSP) and superphosphate + lime (SSP + Ca) (each P source on 4 P levels, with doses of 0, 100, 400 and 1600 mg P 2 O 5 ·kg -1 soil) on the shoot yield of tillering stage spring barley, soil available P (i.e. H 2 O, Olsen, Bray1, Lakanen-Erviö (LE) and ammonium lactate (AL) extractable P contents) were studied in pot experiments set up with acidic sandy soil (Nyírlugos, Hungary) and acidic clay loam soil (Ragály, Hungary), both with low P supplies.  The average spring barley shoot yield at the beginning of shooting was 95% higher on the colloid-rich acidic (pH KCl : 4.5) clay loam soil than on the colloid-poor acidic (pH KCl : 3.8) sandy soil. The differences in the solubility of phosphate rocks showed close correlation to the differences in P responses. On both soils, the correlation between total PR-P added and P responses in spring barley shoot yield was much weaker than that between neutral ammonium citrate soluble PR-P added and P responses in spring barley shoot yield. When phosphate rocks were applied as P sources, the comparison of soil test P methods showed a different picture on the two soils. In the case of the acidic sandy soil (Nyírlugos), the strongly acid LE-P (r² = 0.83) and AL-P (r² =0.74) tests gave the highest correlation coefficients with spring barley responses to P, while on the acidic clay loam soil (Ragály) these were achieved by the Olsen-P (r² = 0.88) and Bray1-P (r² =0.88) methods. 

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