Anthropogenic forcings on shallow landslides triggering

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1 Antropognc forcngs on sallow lansls trggrng Mara Crstna Rull, Poltcnco Mlano

2 Factors wc nflunc or trggr mass movmnt lop atr Antropognc an natural actvts

3 0 < z < < z < z < z < <z< z [ ] ( ) φ sn z z c c c Fs v A ( ) [ ] { } φ sn sn z z c c Fs sat w sat v ] ) ( [ ) ( ( ) [ ] { } φ sn sn z z c c Fs sat w sat A ] ) ( [ ) ( ( ) ( ) [ ] { } φ sn sn z z c Fs sat sat w sat w sat ] ) ( [ ) ( φ br Fs ( ) [ ] { } φ φ sn sn c c Fs sat w sat ] [ )), (mn( ), mn( Prcptaton nuc lansls at basn scal T problm s usually solv n trm of F by couplng an yrologcal mol wt a gomcancal mol Rosso R, Rull M.C. Vannucc G., RR 006

4 Roas ffct on sallow lansls trggrng

5 Hyrologcal Effcts: Roas Effcts Roa surfac an Dtcs Incras Ovrlan Flow Roa Cut Intrcpt ubsurfac Flow Culvrts A nw Cannl to stram ntwork Cannl Ntwork Extnson Q( t) Incras quck scarg Q Q quck bas Q Q Q ran quck cutroa t roa tout roa Incras an antcpaton of pak scarg Volumtrc an Tmng Effct Tm (From mpl, t al. 996)

6 Flow Intrcpton by t ROAD Ranfall Effct on t roa Hp: Imprvous Roa urfac mall rougnss Nglgbl vgtaton transpraton an ntrcpton Hyraulc Analogy: Roa - Cannl a. Outslop b. Inslop c. Crown Q ran I r A roa Runoff gnraton on t roa an on t tc a b c

7 Flow Intrcpton by t ROAD Effct of t roa cut Ovrlan an ubsurfac Flow ntrcpton Q Q Q roacut ovrlan subsurfac nt Q subsurfac Ovrlan-roa Q subsurfac subsurfac l nt ( ) ( ) wt wt nt wt wt

8 Flow Intrcpton by t ROAD T ntrcpt scarg by t roa s rout ownslop troug t culvts Dranag pats Cangs Culvrt connct to t actual ranag ntwork Culvrt connct to pmral cannl Culvrt not connct L Rg L Rc Epmral Cannl L C rvr L D A L Dranag Dnsty D ( L L L L ) Rc Rg A C

9 OUTLET Roa Roa T prsnc of ROAD can mofy contrbutng ara at slct pont

10 Gomcancal Effcts: Roa Influnc Gomtrc Effct Go-mcanc Effct Hyrologc Effct Incras of slop n cutslop an fllslop aras Loss of vgtaton ovraccar co Loa ovuto u to al fllslop trrno rporto Incras of sol watr contnt n ownslop culvrt aras. Cut slop lansls trggrng Fllslop lansls trggrng Dbrs flow Incras of sallow lansls Dbrs flow ar not takn n account n t prsnt analyss

11 allow lansls typology Hllslop ls (nfnt slop analyss) Cutslop ls (tablty maps) Fllslop ls (tablty maps)

12 Hllslop LIDE Infnt lop Analyss ca cv c Fs [ z ] ( z ) sn φ 0 < z < {[ ( z ) ( )] } c cv sat w φ Fs [ ( z ) ] sn sn mn( c, c) Fs ca c Fs [ sat {[ ( ) ( z ) ] } {[ ( )] } [ sat sat sat sat w w (mn( φ, φ)) ] sn sn ( z ) ] sn sn φ < z < z < z < c Fs {[ ( ) ( z ) ( )] } [ sat w sat ( z ) sat sat w ] sn sn φ <z< φ Fs br z Fs most probabl slng surfacs Profontà z rsptto al pano campagna (m)

13 Cutslop an Fllslop LIDE: tablty Carts analyss Hypotss: Crcular falur surfac llslop smpl gomtry ol avng frcton an on ol omognous an sotropc Frcton crcl mto Mor-Coulomb: afty Factor: wt λc φ P tgφ c H q H ' P µ µ ' q τ c σ φ F N P an P CF c H q H µ µ µ q N c H t Taylor, 948

14 BAIN PARTITIONING: stat of t art T mol s a contour-bas mol. It rvs at frst t ranag ntwork startng from t gst contour, tn procs ownslops follow t stpst lns (Mnun t al., 000). Two typ of topograpc lmnts ar consr n flow accountng an routng: Cll : polygon avng two vrtxs on two ajacnt contours an two vrtxs on two stpst lns. It can b trangular wn stpst lns mt. Cannl: mono-mnsonal topograpc lmnt startng at t juncton of stpst lns T ffct of prsnc of ROAD on basn parttonng OUTLET Rull M.C., Rosso R., 008

15 Hyrologcal Fluxs mplf Buckt Mol wt Layrs L L Z Z s Z Z s RF t IN t Unsaturat T aturat LIN Unsaturat T aturat BIN Rock IE t OF t EX t F t IE t EX t F t Rull M.C., Rosso R., AR 007 RF t E t E t aturat aturat BIN Rock OF t F t F t aturat Hyraulc Conuctvty: θ fz θ ry K K 0 ov f m atr Contnt: ( z s z ) ( θ θry ) ( θ ) z θ ry Flux unsaturat -saturat: I st K ubsurfac Flow: sf Infltraton: ln K m ( ) K I s ( θ ry ) z I Prcolaton n t crack Rock: bn K t con ar K ar K f K b I I θ I I m

16 TUDY AREA tuy ara s watrs 3 (3) at t H. J. Anrws Exprmntal Forst, Orgon. Locaton of roas, culvrts, an nstrumntaton ar sown. Elvaton m a.s.l. Ara km Clay ol Macropors n t sol Ks m/s Man Annual Prcp. 300 mm Man ranfall Intnsty 4 mm/ Man Dscarg 5*0 - m 3 /s In orrs of roas wr bult. Ranfall vnt 3-9 Fbruary 996: max ran mm/ Total ran 340mm 6 sallow lansls: 8 llslop 8 fllslop/cutslop Rull M.C., Rosso R., 008

17 Goo Mol rproucton Upslop roa: lansls trggrng s manly u to t gomtrc ffct. Downslop roa: lansls trggrng s manly u to t yrologc ffct.

18 cnaro : ncras of t numbr of culvrts Obsrv sls: T ncras of t numbr of culvrts cras t sls bcaus cras t contrbutng ara at any sngl culvrt

19 cnaro : ncras of t numbr of roas By ncrasng t numbr of roas ramatcally ncras t numbr of sls.

20 Rull M.C.,Boccola D., Rosso R., JoH 006 FIRE INDUCED HALLO LANDLIDE TRIGGERING Fr Forcng on Hyrologcal Procsss Vgtaton covr structon & canopy covr & roots at 0-0 cm of pt Incras ovrlan flow, smnt yl an sallow lansls suscptblty Formaton of a watr rpllnt layr? formaton mcansm? tcknss poston uraton sol typ tmpratur vgtaton covr watr contnt Effcts on sol proprts k ncras n roblty k cras n nfltraton capacty k cras of on

21 THE EVENT OF 8 t OF JULY, 005 T tuy Ara.6 km catcmnt (Ro Caslla) locat n t Pmont, Italy Major Faturs Gology: grantc gnss; n t gst ara, larg zons wt xpos grantc formatons Clmat: mtrranan Ran: manly n May an Octobr (MAP s 300 mm) Vgtaton: Cstnut Hyrograpy: pmral strams Topografy: stp slops, lvaton rang a.s.l. Rull M.C., Rosso R., GRL 006 vr ranfall vnt. About 40 mm of ranfall ropp n lss 30 mnuts (TR 0 yars ) on a prvously burn sol. Mass Movmnt Trggrng (30000 m 3 ) In t pro from t bgnnng of t yar 000 to t ay of t forst fr, 47 ranfall vnts occurr avng or ntnsty or total gratr t ranfall vnt trggrng t mass movmnt of July 005. It mans tat t rol of forst fr n trggrng mass movmnt soul b takn n consraton. Ranfall [mm] Tm [mnuts] On 6 t Marc 005 a svr forst fr occurr n t ara of Ro Caslla burn mor 70% of t stuy ara. 8/07/005 brs-flow 9-0/09/ /09/ /0/ //00

22 To nvstgat t nflunc of cangs n lan covr an sol caractrstcs, from pr- to post-fr contons, on runoff proucton an sallow lansls trggrng, urng a ranstorm Fl Data Vgtaton urvay (Pr; Post an Transnt) ol pt masurmts DPT tst ol typ Pology Gology Hstorcal Ranfall Rcors Hyraulc conuctvty masurmnts (Pr; Post an Transnt) Molng an prctng yrologcal an smntologcal rspons of burn aras Dtrmnstc mol mulaton Runs POT - FIRE To prov a trmnstc framwork for stuyng sallow lansls suscptblty n t ffrnt tmporal scnaros POT- FIRE/ 6 MONTH PRE- FIRE Frcton Angl [ ] aturat ol pc. gt [KN/m³] Coson [KPa] Apparnt Coson [Kpa] BM Paramtrs POT-FIRE TRANIENT/ 6 MONTH aftr t forst fr PRE-FIRE ol pt upslop [m].5.5 ol pt ownslop [m].5 3 Ks upslop [m/s] Ks ownslop [m/s] / / / / / / Multplng factor for orzontal K s [-] Rat of cay n K s wt pt [-] atur sol watr contnt θ [- ] Rsual sol watr contnt θ N [-] Intal satur stor of t buckt [%] Intal sol watr contnt - upslop [-] Intal sol watr contnt - ownslop [-] POT-FIRE TRANIENT/ 6 MONTH PRE-FIRE Mannng coffcnt - lops [s m -/3 ] 0.04/ / /0.04 Mannng coffcnt - Cannls - upslop [s m -/3 ] Mannng coffcnt - Cannl ownslop[ s m -/3 ] Crtcal upport Ara [-] Cannl t calng Factor [- ] Outlt Flow t [m] Tm tp for t Knmatc av [s]

23 Tmporal cnaros - pr-fr: t pro of tm bfor t forst fr occurr - post-fr: t pro from t tm wn t fr stngus to t n of t sprng n t subsqunt yar - transnt: t pro of tm rqur for t rstoraton of t sol, followng fr nuc sturbanc TRANIENT POT FIRE POT FIRE PRE FIRE Rull M.C., Rosso R., AR 007

24 Conclusons: Antropognc an natural actvts lk roas an forst frs can strongly nflunc t yrologc rspons an sallow lansls suscptblty of uplan catcmnts! For stuyng antropognc an natural actvts nflunc on sallow lansls trggrng t s ncssary corrctly valuat t ffcts of ts actvts on t yrologcal fluxs (gnraton an rcton). For stuyng antropognc an natural actvts nflunc on sallow lansls trggrng t s ncssary corrctly slct t gomcancal mol! THANK YOU!

25 ( ) [ ] ( ) [ ] θ φ ω ω ' r r s r r s G G F > ; * ln f, ; * ln f, xp * p p A p p A A p p ξ ξ ξ ω a Tb p snθ * ( ) r A ω /z ξ (p*/z)t

26 Prcptaton trsol for slop nstablty Couplng llslop yrology wt gomcancs yls lansl trggrng by prcptaton ( ) ( ) t az Tb t az Tb z G a b T t p r r r r s CR θ θ φ θ φ θ θ sn xp sn xp ' ' ) ( sn Tmporal scal of llslop voluton T ranfall rat p F tat can b xc wt a probablty of ( F) n a yar ( ) ) ( n F F t x m t p p CR p CR (t) ( ) ) ( sn xp sn xp ' ' ) ( sn n F r r r r s t m x t az Tb t az Tb z G a b T θ θ φ θ φ θ θ

27 p CR an pf [mm/] a/b 00 m a/b 50 m a/b 00 m 00 a/b 00 m TR 500 ya TR 70 yars TR 5 yars t [] 00 Maps of Mttman Rg catcmnt sowng sallow lanslng pron aras n trm of rturn pro of potntal falur consrng ntal conton of stabl pzomtrc at t pt of brock, (0) 0 an (0) 0.5, φ 45, T 65 m/, ρs 600 kg/m3 an Gs.60.

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