ࡱ>    >+ !"$%&'()*=-./0123456789:;^?@ABCDEFGHIJKLNOPQRSTUVWXYZ[\]Root Entry Ѕ[ ITEM000  F0xDЅ[1Table#CompObjj՜.+,0 hp|   _ A  Title  FMicrosoft Word Document MSWordDocWord.Document.89q%F\Object F4dMicrosoft Word DocumentD:\Youngs Bay final data\Stream reports\Lewis and Clark Tribs\Barrett Creek Report.docWordDocument"SummaryInformation( DocumentSummaryInformation8Oh+'0h   $ 0 <HPX`ssBenenNormal Todd Boswello2ddMicrosoft Word 10.0@vA@_D}@>j@Gf5@ cbjbj22 "XXc 6666666      66666666  $ RH 6 66  6666   j6666   w 66w 6* ,;  w 0 w d (dw J$n6666d6w 6| `dS666     Upper Nehalem Watershed Habitat Assessment Stream Report STREAM: Derby Creek SUBBASIN: Upper Nehalem River DATES: April 10, 2006 SURVEY CREW: Todd Boswell, Mark McLaughlin REPORT PREPARED BY: Ben Walczak GENE CONSERVATION GROUP: 1-NC UTM COORDINATES: Start 0470571 E & 5062326 N End 0470305 E & 5062633 N USGS MAPS: Cochran GENERAL DESCRIPTION: The Derby Creek winter habitat survey begins at its confluence with the Nehalem River and extends 293 meters. One reach was designated based on: Valley form. In the reach Riffles (43%) and Rapids (40%) dominated the habitat, while Sand (17%), Gravel (29%), and Cobble (42%) were the dominant substrate types. The survey begins at the confluence with the Nehalem River above Reeher Park (ODF) near the town of Timber. An ODFW Spawning Survey sign was not noted and the habitat is marginal with high gradient riffles from the start. The stream gradient never really levels out. The survey was ended quickly due to lack of pools, gravel, and habitat conductive for coho. REACH DESCRIPTIONS: REACH 1: Length 291 meters. The channel is constrained by hillslopes in a narrow valley. The average valley width index is 1.9. Land use for the reach is large timber. A sub dominant land use of second growth timber was also noted. The average unit gradient is 5.1%. The channel characteristics include: primary 291m and secondary 2m. No pools were greater than 1 meter deep. There was one key piece of LWD, which averages to 0.3 pieces per 100m. The vegetation is based on one riparian transect. The trees found most frequently in the riparian zone were mostly mixed sizes of deciduous ranging from 30 50 cm dbh, with some conifers 30 50 cm dbh. This survey begins at the confluence with the Nehalem River. This short survey consists of high gradient riffles and rapids with a lack of spawning gravel throughout. There was also a lack of pools. No fry were observed during the survey. The survey ended at a cascade above a number of small boulders. The stream becomes very constrained by hillslopes above the endpoint. There is poor LWD project potential with poor access for industrial equipment. This steep stream also has a narrow valley further reducing the potential to increase complexity. The riparian has a great mix of conifers and alders. So, a planting projects is not necessary. CchM5CJ\hM/BCYZyz  1 Q R f g | } ! # 7 8 !!!!!!!!!!!!!!!!!!!!!!!!!!!!!c8 A B NOc!!!!!!! 1h/ =!"#$%@@@ NormalCJ_HaJmH sH tH DAD Default Paragraph FontVi@V  Table Normal :V 44 la (k@(No List c  z zc /BCYZyz1QRfg|}!#78ABNOe 0000000000000 000000 00000 000 00 00 0 000p0c 8 c c NyNyNy<NyT#Ny2Ny\Ny\Ny2Nyd2NyNyNyeeks e    jrxx e   8*urn:schemas-microsoft-com:office:smarttagsCity= *urn:schemas-microsoft-com:office:smarttags PlaceType= *urn:schemas-microsoft-com:office:smarttags PlaceName9 *urn:schemas-microsoft-com:office:smarttagsplace   w/9W ` e 8 b e M8 a b e W ` e Todd Landon BoswellTodd Landon BoswellTodd Landon BoswellTodd Landon BoswellTodd Landon BoswellTodd Landon BoswellTodd Landon BoswellTodd Landon BoswellTodd Landon BoswellMark McLaughlinM@a a ӒZZa a c @@UnknownGz Times New Roman5Symbol3& z Arial"qhdd ff!r4d_ _ 3H(?MBen Todd BoswellOle 5OlePres000,, ITEM000ODS ITEM000FMT;lX   ."System8$r0E -@Times New Roman-  2 Z -- 2  , 2 , , 2 X ,@Times New Roman-J2 *Upper Nehalem Watershed Habitat AssessmentTAA44T4A:!4`u;'44.A3A[;@!&;'T--4..`4A' 2  > 2 e , 2 e, , 2 eX , 2 e , 2 e ,2 e Stream ReportA'44;`T4A;4' 2 e > 2  ?-)2 _STREAM: Derby Creek8=C=HYH,!30C",,3 2 _ 2 _ - 2  -82 ESUBBASIN: Upper Nehalem River8HBBH9 HH22,!H,3,,NC2,! 2 E . 2  -.2 +DATES: April 10, 2006HH==8H2!222222 2 + - 2  -L2 +SURVEY CREW: Todd Boswell, Mark McLaughlin8HCH=HCC=_=221B2'H,Y,!2Z-<,3222 2 ^ - 2  -;2  REPORT PREPARED BY: Ben WalczakC=8HC=8C<8HC=HBHB,2_,,-,2 2  . 2 j -/2 GENE CONSERVATION GROUP:H=H=CHH8=CHH> IHHCHH8 2  ' 2 12 2 -!2 /NCHC 2  - 2 P -#2 UTM COORDINATES:H=YCHHCI HH==8 2  2 Start 8,! 2 2.2  0470571 E & 5062326 N 2222222=M2232222H 2   - 2 6 , 2 6, , 2 6X , 2 6 ,2 6End =22 2 6j2,2 6 0470305 E & 5062633 N2222222=M2232222H 2 6  - 2  -(2  USGS MAPS: Cochran3H8H8YH88C2,2!,2 2   - 2  -)2  GENERAL DESCRIPTION:H=H=CI<H=8CD8>!HH 2   - 2 u  - 2  ,2 ,PThe Derby Creek winter habitat survey begins at its confluence with the Nehalem =2,H,!40C",,2H2-!2,2,'2!2.02-12',',22!2,2,,H22,H-2,,NV2 [ 2River and extends 293 meters. One reach was designC2,!,22,3,22'222N,,!'H2,!,-,2H,'3,'12A2 [ A$ated based on: Valley form. In the ,,22,',222I,.0"2!N23,2 Ureach Riffles (43%) and Rapids (40%) dominated the habitat, while Sand (17%), Gravel 3!,,,2C"!,'!22T!,22C,22'!22S!22N2,,32,2,2,H2,8,22"22S!H",2,b2 A :(29%), and Cobble (42%) were the dominant substrate types.!22S!,22C222,!22T!H,",2,22N2,2'22'!,,03,' 2 A  . 2  -|2 ' KThe survey begins at the confluence with the Nehalem River above Reeher Para=2,'2!2.02-12',2,,22!2,2-,H22,H,3,,NC2,!,222,C-,2-"8,!2 ' S k (ODF) 2!HI7!2 Mnear the town of Timber. An ODFW Spawning Survey sign was not noted and the e2,,!2,2H23!=N2,!H2HH7_82,H23182!2.0'12H,'2222,2-222,2 Zhabitat is marginal with high gradient riffles from the start. The stream gradient never 2,2,'N,!13,H22121!,2,2!!!,'!!2N2,',!=2,'!-,N1!,3,22,2,!2 Qreally levels out. The survey was ended quickly due to lack of pools, gravel, anv!,,0,2,'22=2,'2"2-0H,',23,222,2032,2,,22!222'1!,3-,22 t d habitat 22,2,,2 conductive for coho. ,2222,2,!2!,222 2 j . 2 f , 2 f, -(2 REACH DESCRIPTIONS:.C=HCHH=8CD8> HI8 2 J , 2 L -2 REACH 1:C=HCH2 2  - 2 2 - 2  ,2 ,Length :<,312 2 _2}2 L 291 meters. The channel is constrained by hillslopes in a narrow valley. 222N,,!'=3,,2,23,',22'!,2,2302'22,'2,2,"!2H2,-02 WThe average valley width index is 1.9. Land use for the reach is large timber. A sub =2,,2-!-1,3,.0H2322,3'22;,222(,"2!2,!-,,2',"2,N2,!H'22&2 dominant land use 22N2,2,222',t2 Fof second growth timber was also noted. The average unit gradient is 2!',-2221!3H2N2,!H,','222,2=2,,2-!-1,321!,2,2'2 U5.1%. The channel characteristics include: primary 291m and secondary 2m. No pools b22S=2,,3,22,,3,!-,,!','2,22,2!N,"0222N,22(,,222-#03NH2222'2 qWwere greater than 1 meter deep. There was one key piece of LWD, which averages to 0.3 H,!,2!,,,!2,22N,-"2,,2=2-!,I,'22,2-02-,,2!<_HH2,2-2,!-1,'222 2 pieces per 1002,,,'2-!222}2 ALm. The vegetation is based on one riparian transect. The trees found most N=2,2-1,,22'2,',22222,"2,!,2!,2'-,=2,",-'!2222N2'2 WUfrequently in the riparian zone were mostly mixed sizes of deciduous ranging from 30 3!!,22,2022,!2-!,2-22,H,!,N2'0N3,2'-,'2!2,,2222'!,3131"!2N22 2 W 2 2 W  =2 !50 cm dbh, with some conifers 30 h22,N222H2'2N,,22!,!'22 2 f22   50 cm dbh. 22,N222 2 {\rtf1\ansi\ansicpg1252\uc1\deff0\stshfdbch0\stshfloch0\stshfhich0\stshfbi0\deflang1033\deflangfe1033{\fonttbl{\f0\froman\fcharset0\fprq2{\*\panose 02020603050405020304}Times New Roman;}{\f35\fswiss\fcharset0\fprq2{\*\panose 020b0604030504040204}Tahoma;} {\f36\froman\fcharset238\fprq2 Times New Roman CE;}{\f37\froman\fcharset204\fprq2 Times New Roman Cyr;}{\f39\froman\fcharset161\fprq2 Times New Roman Greek;}{\f40\froman\fcharset162\fprq2 Times New Roman Tur;} {\f41\froman\fcharset177\fprq2 Times New ITEM000FMT#3 FITEM000FMTRich Text Format8<Ole  OlePres000M, #3Rich Text Formatat;lXp!Roman (Hebrew);}{\f42\froman\fcharset178\fprq2 Times New Roman (Arabic);}{\f43\froman\fcharset186\fprq2 Times New Roman Baltic;}{\f44\froman\fcharset163\fprq2 Times New Roman (Vietnamese);} {\f386\fswiss\fcharset238\fprq2 Tahoma CE;}{\f387\fswiss\fcharset204\fprq2 Tahoma Cyr;}{\f389\fswiss\fcharset161\fprq2 Tahoma Greek;}{\f390\fswiss\fcharset162\fprq2 Tahoma Tur;}{\f391\fswiss\fcharset177\fprq2 Tahoma (Hebrew);} {\f392\fswiss\fcharset178\fprq2 Tahoma (Arabic);}{\f393\fswiss\fcharset186\fprq2 Tahoma Baltic;}{\f394\fswiss\fcharset163\fprq2 Tahoma (Vietnamese);}{\f395\fswiss\fcharset222\fprq2 Tahoma (Thai);}}{\colortbl;\red0\green0\blue0;\red0\green0\blue255; \red0\green255\blue255;\red0\green255\blue0;\red255\green0\blue255;\red255\green0\blue0;\red255\green255\blue0;\red255\green255\blue255;\red0\green0\blue128;\red0\green128\blue128;\red0\green128\blue0;\red128\green0\blue128;\red128\green0\blue0; \red128\green128\blue0;\red128\green128\blue128;\red192\green192\blue192;}{\stylesheet{\ql \li0\ri0\widctlpar\aspalpha\aspnum\faauto\adjustright\rin0\lin0\itap0 \fs24\lang1033\langfe1033\cgrid\langnp1033\langfenp1033 \snext0 Normal;}{\*\cs10 \additive \ssemihidden Default Paragraph Font;}{\*\ts11\tsrowd\trftsWidthB3\trpaddl108\trpaddr108\trpaddfl3\trpaddft3\trpaddfb3\trpaddfr3\trcbpat1\trcfpat1\tscellwidthfts0\tsvertalt\tsbrdrt\tsbrdrl\tsbrdrb\tsbrdrr\tsbrdrdgl\tsbrdrdgr\tsbrdrh\tsbrdrv \ql \li0\ri0\widctlpar\aspalpha\aspnum\faauto\adjustright\rin0\lin0\itap0 \fs20\lang1024\langfe1024\cgrid\langnp1024\langfenp1024 \snext11 \ssemihidden Normal Table;}{\s15\ql \li0\ri0\widctlpar\aspalpha\aspnum\faauto\adjustright\rin0\lin0\itap0 \f35\fs16\lang1033\langfe1033\cgrid\langnp1033\langfenp1033 \sbasedon0 \snext15 \ssemihidden \styrsid15794406 Balloon Text;}}{\*\rsidtbl \rsid5119079\rsid8473990\rsid15794406} \widowctrl\ftnbj\aenddoc\noxlattoyen\expshrtn\noultrlspc\dntblnsbdb\nospaceforul\formshade\horzdoc\dgmargin\dghspace180\dgvspace180\dghorigin1800\dgvorigin1440\dghshow1\dgvshow1 \jexpand\viewkind1\viewscale100\pgbrdrhead\pgbrdrfoot\splytwnine\ftnlytwnine\htmautsp\nolnhtadjtbl\useltbaln\alntblind\lytcalctblwd\lyttblrtgr\lnbrkrule\rsidroot8473990 \fet0\sectd \linex0\endnhere\sectlinegrid360\sectdefaultcl\sftnbj {\*\pnseclvl1 \pnucrm\pnstart1\pnindent720\pnhang {\pntxta .}}{\*\pnseclvl2\pnucltr\pnstart1\pnindent720\pnhang {\pntxta .}}{\*\pnseclvl3\pndec\pnstart1\pnindent720\pnhang {\pntxta .}}{\*\pnseclvl4\pnlcltr\pnstart1\pnindent720\pnhang {\pntxta )}}{\*\pnseclvl5 \pndec\pnstart1\pnindent720\pnhang {\pntxtb (}{\pntxta )}}{\*\pnseclvl6\pnlcltr\pnstart1\pnindent720\pnhang {\pntxtb (}{\pntxta )}}{\*\pnseclvl7\pnlcrm\pnstart1\pnindent720\pnhang {\pntxtb (}{\pntxta )}}{\*\pnseclvl8\pnlcltr\pnstart1\pnindent720\pnhang {\pntxtb (}{\pntxta )}}{\*\pnseclvl9\pnlcrm\pnstart1\pnindent720\pnhang {\pntxtb (}{\pntxta )}}\pard\plain \ql \li0\ri0\widctlpar\aspalpha\aspnum\faauto\adjustright\rin0\lin0\itap0 \fs24\lang1033\langfe1033\cgrid\langnp1033\langfenp1033 {\insrsid8473990 \par }\pard \ql \li0\ri0\widctlpar\aspalpha\aspnum\faauto\adjustright\rin0\lin0\itap0 {\insrsid8473990 \tab \tab \tab }{\b\fs28\insrsid8473990 Upper Nehalem Watershed Habitat Assessment \par \tab \tab \tab \tab \tab Stream Report \par \par }\pard \ql \li0\ri0\widctlpar\aspalpha\aspnum\faauto\adjustright\rin0\lin0\itap0 {\insrsid8473990 STREAM: Derby Creek\tab \par \par SUBBASIN: Upper Nehalem River \par \par DATES: April 10, 2006 \par \par SURVEY CREW: Todd Boswell, Mark McLaughlin \par \par REPORT PREPARED BY: Ben Walczak \par \par GENE CONSERVATION GROUP:\tab 1-NC \par \par UTM COORDINATES:\tab Start \endash 0470571 E & 5062326 N \par \tab \tab \tab \tab End \endash 0470305 E & 5062633 N \par \par USGS MAPS: Cochran \par \par GENERAL DESCRIPTION: \par \par }\pard \ql \li0\ri0\widctlpar\aspalpha\aspnum\faauto\adjustright\rin0\lin0\itap0 {\insrsid8473990 \tab The Derby Creek winter habitat survey begins at its confluence with the Nehalem River and extends 293 meters. One reach was design ated based on: Valley form. In the reach Riffles (43%) and Rapids (40%) dominated the habitat, while Sand (17%), Gravel (29%), and Cobble (42%) were the dominant substrate types. \par }\pard \ql \li0\ri0\widctlpar\aspalpha\aspnum\faauto\adjustright\rin0\lin0\itap0 {\insrsid8473990 \par }\pard \ql \li0\ri0\widctlpar\aspalpha\aspnum\faauto\adjustright\rin0\lin0\itap0 {\insrsid8473990 The survey begins at the confluence with the Nehalem River above Reeher Par k (ODF) near the town of Timber. An ODFW Spawning Survey sign was not noted and the habitat is marginal with high gradient riffles from the start. The stream gradient never really levels out. The survey was ended quickly due to lack of pools, gravel, a nd habitat conductive for coho. \par }\pard \ql \li0\ri0\widctlpar\aspalpha\aspnum\faauto\adjustright\rin0\lin0\itap0 {\insrsid8473990 \tab \par REACH DESCRIPTIONS: \par \par REACH 1: \par \par }\pard \ql \li0\ri0\widctlpar\aspalpha\aspnum\faauto\adjustright\rin0\lin0\itap0 {\insrsid8473990 \tab Length \endash 291 meters. The channel is constrained by hillslopes in a narrow valley. The average valley width index is 1.9. Land use for the reach is large timber. A sub dominant land use of second growth timber was also noted. The average unit gradient is 5.1%. The channel characteristics include: primary 291m and secondary 2m. No pools were greater than 1 meter deep. There was one key piece of LWD, which averages to 0.3 pieces per 10 0m. The vegetation is based on one riparian transect. The trees found most frequently in the riparian zone were mostly mixed sizes of deciduous ranging from 30 \endash 50 cm dbh, with some conifers 30 \endash 50 cm dbh. \par }\pard \ql \li0\ri0\widctlpar\aspalpha\aspnum\faauto\adjustright\rin0\lin0\itap0 {\insrsid8473990 \par }\pard \ql \li0\ri0\widctlpar\aspalpha\aspnum\faauto\adjustright\rin0\lin0\itap0 {\insrsid8473990 This survey begins at the confluence with th e Nehalem River. This short survey consists of high gradient riffles and rapids with a lack of spawning gravel throughout. There was also a lack of pools. No fry were observed during the survey. The survey ended at a cascade above a number of small bo ulders. The stream becomes very constrained by hillslopes above the endpoint. \par }\pard \ql \li0\ri0\widctlpar\aspalpha\aspnum\faauto\adjustright\rin0\lin0\itap0 {\insrsid8473990 \par }\pard \ql \li0\ri0\widctlpar\aspalpha\aspnum\faauto\adjustright\rin0\lin0\itap0 {\insrsid8473990 There is poor LWD project potential with poor access for industrial equipment. This steep stream also has a narrow valley further reducing the potential to increase complexity. The riparian has a great mix of conifers and alders. So, a planting projects is not necessary. }}S: CochrankH8H8YH88C2,2!,2 2  C- 2 5  C-)2 GENERAL DESCRIPTION:H=H=CH;H=8CC8=HH 2  C- 2   C- 2  C;lX   ."System8$r0E -@Times New Roman-  2 Z -- 2  , 2 , , 2 X ,@Times New Roman-J2 *Upper Nehalem Watershed Habitat AssessmentTAA44T4A:!4`u;'44.A3A[;@!&;'T--4..`4A' 2  > 2 e , 2 e, , 2 eX , 2 e , 2 e ,2 e Stream ReportA'44;`T4A;4' 2 e > 2  ?-)2 _STREAM: Derby Creek8=C=HYH,!30C",,3 2 _ 2 _ - 2  -82 ESUBBASIN: Upper Nehalem River8HBBH9 HH22,!H,3,,NC2,! 2 E . 2  -.2 +DATES: April 10, 2006HH==8H2!222222 2 + - 2  -L2 +SURVEY CREW: Todd Boswell, Mark McLaughlin8HCH=HCC=_=221B2'H,Y,!2Z-<,3222 2 ^ - 2  -;2  REPORT PREPARED BY: Ben WalczakC=8HC=8C<8HC=HBHB,2_,,-,2 2  . 2 j -/2 GENE CONSERVATION GROUP:H=H=CHH8=CHH> IHHCHH8 2  ' 2 12 2 -!2 /NCHC 2  - 2 P -#2 UTM COORDINATES:H=YCHHCI HH==8 2  2 Start 8,! 2 2.2  0470571 E & 5062326 N 2222222=M2232222H 2   - 2 6 , 2 6, , 2 6X , 2 6 ,2 6End =22 2 6j2,2 6 0470305 E & 5062633 N2222222=M2232222H 2 6  - 2  -(2  USGS MAPS: Cochran3H8H8YH88C2,2!,2 2   - 2  -)2  GENERAL DESCRIPTION:H=H=CI<H=8CD8>!HH 2   - 2 u  - 2  ,2 ,PThe Derby Creek winter habitat survey begins at its confluence with the Nehalem =2,H,!40C",,2H2-!2,2,'2!2.02-12',',22!2,2,,H22,H-2,,NV2 [ 2River and extends 293 meters. One reach was designC2,!,22,3,22'222N,,!'H2,!,-,2H,'3,'12A2 [ A$ated based on: Valley form. In the ,,22,',222I,.0"2!N23,2 Ureach Riffles (43%) and Rapids (40%) dominated the habitat, while Sand (17%), Gravel 3!,,,2C"!,'!22T!,22C,22'!22S!22N2,,32,2,2,H2,8,22"22S!H",2,b2 A :(29%), and Cobble (42%) were the dominant substrate types.!22S!,22C222,!22T!H,",2,22N2,2'22'!,,03,' 2 A  . 2  -|2 ' KThe survey begins at the confluence with the Nehalem River above Reeher Para=2,'2!2.02-12',2,,22!2,2-,H22,H,3,,NC2,!,222,C-,2-"8,!2 ' S k (ODF) 2!HI7!2 Mnear the town of Timber. An ODFW Spawning Survey sign was not noted and the e2,,!2,2H23!=N2,!H2HH7_82,H23182!2.0'12H,'2222,2-222,2 Zhabitat is marginal with high gradient riffles from the start. The stream gradient never 2,2,'N,!13,H22121!,2,2!!!,'!!2N2,',!=2,'!-,N1!,3,22,2,!2 Qreally levels out. The survey was ended quickly due to lack of pools, gravel, anv!,,0,2,'22=2,'2"2-0H,',23,222,2032,2,,22!222'1!,3-,22 t d habitat 22,2,,2 conductive for coho. ,2222,2,!2!,222 2 j . 2 f , 2 f, -(2 REACH DESCRIPTIONS:.C=HCHH=8CD8> HI8 2 J , 2 L -2 REACH 1:C=HCH2 2  - 2 2 - 2  ,2 ,Length :<,312 2 _2}2 L 291 meters. The channel is constrained by hillslopes in a narrow valley. 222N,,!'=3,,2,23,',22'!,2,2302'22,'2,2,"!2H2,-02 WThe average valley width index is 1.9. Land use for the reach is large timber. A sub =2,,2-!-1,3,.0H2322,3'22;,222(,"2!2,!-,,2',"2,N2,!H'22&2 dominant land use 22N2,2,222',t2 Fof second growth timber was also noted. The average unit gradient is 2!',-2221!3H2N2,!H,','222,2=2,,2-!-1,321!,2,2'2 U5.1%. The channel characteristics include: primary 291m and secondary 2m. No pools b22S=2,,3,22,,3,!-,,!','2,22,2!N,"0222N,22(,,222-#03NH2222'2 qWwere greater than 1 meter deep. There was one key piece of LWD, which averages to 0.3 H,!,2!,,,!2,22N,-"2,,2=2-!,I,'22,2-02-,,2!<_HH2,2-2,!-1,'222 2 pieces per 1002,,,'2-!222}2 ALm. The vegetation is based on one riparian transect. The trees found most N=2,2-1,,22'2,',22222,"2,!,2!,2'-,=2,",-'!2222N2'2 WUfrequently in the riparian zone were mostly mixed sizes of deciduous ranging from 30 3!!,22,2022,!2-!,2-22,H,!,N2'0N3,2'-,'2!2,,2222'!,3131"!2N22 2 W 2 2 W  =2 !50 cm dbh, with some conifers 30 h22,N222H2'2N,,22!,!'22 2 f22   50 cm dbh. 22,N222 2  .-NANI .-NANI