Monografija - Geološki zavod Slovenije

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Marko KomacNapoved verjetnosti pojavljanja plazov z analizo satelitskih in drugih prostorskih podatkovnajvečjo razliko med pričakovanimi in dejanskimi vrednostmi pojavov pa je, tako kotpri K-S testu, opaziti v četrtem razredu (Preglednica 4.33). Z oddaljenostjo odgeloških mej dejanske vrednosti padajo in so pod pričakovanimi (Slika 4.46).Št. plazov70065060055050045040035030025020015010050Spremenljivka Odd_gmeja_ln; porazdelitev: lognormalnaKolmogorov-Smirnov d = 0,1178551, p < 0,0100,000 0,750 1,500 2,250 3,000 3,750 4,500 5,250 6,000 6,750 7,500 8,250 9,0000,375 1,125 1,875 2,625 3,375 4,125 4,875 5,625 6,375 7,125 7,875 8,625Logaritem oddaljenosti od geoloških mej (zgornja meja razreda)PričakovanoSlika 4.45 – Kumulativna krivulja logaritmiranih podatkov o oddaljenosti lokacij plazovod geoloških mej. S črto je prikazana teoretična porazdelitev glede na vrednosti ozadja ( x= 5,502932, δ 2 = 1,83727).Preglednica 4.32 – Logaritmirane vrednosti spremenljivke “Odd_gmej” in razdelitev vrazrede.x min x max x sLogaritmirane vrednosti oddaljenosti odgeoloških mej na lokacijah plazov (vzorec)–1,309 7,65646 4,9877 1,406434Logaritmirane vrednosti oddaljenosti ozadjaod geoloških mej (populacija)- 8,69007 5,502932 1,355461Razred Oznaka Razred Oznaka Razred Oznaka< 0,91629 1 3–4 4 6–7 70,91629–2 2 4–5 5 7–8 82–3 3 5–6 6 8–9 9Preglednica 4.33 – χ 2 test vpliva oddaljenosti od geoloških mej na pojavljanje vseh plazov.Vsi plazovi – “Odd_gmej_ln”χ 2 = 73,79374 df = 8 p < 0,0000Razred Razdalja (m) Dejan. plazov Prič. plazov D – P χ 2 = (D-P) 2 /P
Marko KomacNapoved verjetnosti pojavljanja plazov z analizo satelitskih in drugih prostorskih podatkovVsi plazovi – “Odd_gmej_ln”χ 2 = 73,79374 df = 8 p < 0,0000Razred Razdalja (m) Dejan. plazov Prič. plazov D – P χ 2 = (D-P) 2 /P6–7 403,4–1096,6 132 163,5 –31,5 6,0912487–8 1096,6–2981 30 39,4 –9,4 2,2539158–9 2981–8103,1 0 1,3 –1,3 1,2973Σ 614 614 0 73,79374250Vsi plazovi200Št. plazov150100500
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Monografija - Geološki zavod Slovenije

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