Počet záznamov: 1
ozón
SYS d010126 LBL 00000nz--a2200000o--4500 005 20250606214715.2 008 990101|||anznnbabn-----------|-a|a------ 040 $b slo $a DNLM $d BA006 065 $a D01.362.670.600 066 $a 01 $c 03 150 $a ozón $x AD $x AE $x AG $x AI $x AN $x BL $x CF $x CH $x CL $x CS $x EC $x HI $x IM $x IP $x ME $x PD $x PK $x PO $x RE $x SD $x ST $x TO $x TU $x UR $2 slo 550 $7 sllk_us_auth*d010083 $Y Oxidants, Photochemical $w P $a oxidanty fotochemické 680 9-
$i The unstable triatomic form of oxygen, O3. It is a powerful oxidant that is produced for various chemical and industrial uses. Its production is also catalyzed in the ATMOSPHERE by ULTRAVIOLET RAY irradiation of oxygen or other ozone precursors such as VOLATILE ORGANIC COMPOUNDS and NITROGEN OXIDES. About 90% of the ozone in the atmosphere exists in the stratosphere (STRATOSPHERIC OZONE). $2 eng 680 $a OZONE DEPLETION is also available $2 eng 750 -2
$a Ozone $2 eng 980 $x M
Počet záznamov: 1