<71\\
'-
Presentations given at the Annual Meeting of the
Intermountain Forest Tree Nutrition cooperative
April, 1985
Table of Contents
Two-year growth response results for the 1981 and 1982 installations using the experimental design.
By Peter Mika.
A predictive model of basal area growth response to nitrogen treatments. By Jim Moore.
Additional comparisons of growth response to treatment by soil parent materials using the predictive model. By Jim Moore.
1
28
53
I. Mineralizable-nitrogen as a predictor of
treatment response. II. Other mineral nutrients--
are they also limiting growth! By Kurt Pregitzer. 56 Soil moisture holding capacity for selected parent
materials. By Jim Mital. 79
Douglas-fir height growth and site index curves-- testing and refinement using IFTNC stem analysis data. By Jim VanderPloeg.
Information requirements for an operational fertilization program. By John Olson.
Applied research needs. By John Shumway.
Basic research needs and opportunities.
By John Mandzak.
83
111
125
127
Peter Mika, Data Analyst I.P'.T.N.C.
I. Review of experimental set-up
A. Distribution of installations by reqion and year B. samplinq qoals
1. 2nd qrowth, even-aqed, manaqed stands of Df 2. Ranqe of aqes, tree sizes, densities, site conditions
Conditions sampled:
Range Mean
Aqe 27 to 100 65 years
SA 48 to 272 142 ft2/A
DSH 5.8 to 15.3 10.3 inches
site Index 37.1 to 108.0 68.7 ft @50 yrs
% Df 87.5%
-"-
Plot set-up
II. Results from analysis of experimental desiqn A. Model #1
1. OVerall model statistics
2. Details on factors influencinq treatment response a. Reqional differences (at SA = 150 ft2/A)
(i) Absolute 2 year BAI by treatment and reqion
2
Good qeneral qrowth in N Idaho Poor qrowth in HE Oreqon
General increase from control to N treatment across all reqions (ii) Difference between control and N
treatment by reqion
Larqe response of N. Idaho and Central Washinqton
Larqe chanqe from 200 to 400 in Central Washinqton
(iii) %chanqe [(treatment-control/control]
Relative response about the same over all reqions, except for Central Washinqton
b. SA differences
(i) %response decreases as initial BA
increases
(ii) 400 # response seems to converqe to
200# response at hiqher SA ( 200
ft2/A)
3. Details on factors influence underlyinq qrowth rates
a. SA differences
(i) OVerall, as SA increases, qrowth/acre also increases - effect of increased stockinq level
(ii) Yearly differences
"
.,
3
1981 - decreasinq rate of BAI/BA at hiqher BA
1982 - linear across the ranqe of BA's b. Year differences - vary by reqion
(i) North Idaho, Central Idaho, HE Oreqon, Central Washinqton - hiqher qrowth rates on 1982 installation
(ii) HE Washinqton - growth rates similar in both years
(iii) Montana - hiqher qrowth rates on 1981 installation
SCI Hodel #2
Reqion x treatment and BA x treatment replaced by Min N x treatment
1. OVerall model statistics
2. Factors influencinq treatment response a. Min N differences
(i) Converqence of treatment response to control levels as Min N increases (ii) Converqence of 400# to 200# on Min N
increases
3. Factors influencinq underlyinq qrowth rates a. Min N
(i) Growth on control plots shows trend of increasinq qrowth with increasinq Min-
N
(ii) Basically no trend (zero slope) for SAX versus Min N on treated plots
4
Nur·1BER OF INSTALLATIONS
YEAR OF INSTALLMENT
REGION 1 1981 1982 TOTAL
NORTHERN IDAHO S 14 19
CENTRAL IDAHO 3 S 13
MONTANA 8 8 16
NE OREGON 6 2 3
CENTRAL WASHINGTON 9 9 ·18
NE WASHINGTON 9 7 16
"'" TOTAL lIS LJS 90
5
DESIGN NODEl 1
IN
(BAD
=F ( YEAR , REGION , YEAR X REGION, INSTAllATION ( YEAR REGION )
BLOCK ( YEAR REGION INSTAllATION ) TREATMENT
REGION X TREATMENT
6
BA X TREATMENT BA2 X TREATMENT
BA X YEAR BA2 X YEAR )
R2
=0.9025 f1SE = 0.0243 cv -
~...... 86
11,o) )I j .; ;) ) ) ) J j j
2 YEAR BASAL AREA INCREMENT
BY TREATMENT AND REGION BAI
20
15
5
o
II - I
I I
I : J.lJ__ I
C 2 4 0 0 0
N 0 0 T
C 2 4 C 2 4
a
f2J f2Ja
0 f2JN f2J 0 N f2J f2J
T T
C 2 4 C 2 4 C 2 4 C 2 4 0 0 0 0 0 0 0 0 0 0 0 0 N 0 0 N 0 0 N 0 0 N 0 0
T T T T TRTMENT
MEAN N 1D MONT C 1D NE OR C UA NE UA REGION
-..J~ ) ) ) ) j ~ ) ) ii j
SAl INCREASE OVER CONTROL
BY TREATMENT AND REGION RESPONSE
5
TRTMENT
2 4
o
0o
02 4
o
fao
02 4
fa 0
o
02 4
o
0o
02 4
o
0o
0 2 4o
0o
02 4
o
0o
02
j
I I
I :
o
~lJ t.. l
4
MEAN N 1D MONT C 1D NE OR C UA NE UA REGION
enJ )
iii
;)
)
}
.Jl
}
j )
....
)
".
2 YEAR BASAL AREA INCREMENT
G£OGRAPHICAl R£GIONbC£NTRAl IDAHO
18
8~
6 B A I
i
\0
~ 1
98/, 200lBs
~
1982,CONTROL
~
1982, 400lBs
..." 19
8', CONTROL fJ-s-{J 1981, 400
las
*-*-.
1982, 2aelas
1-~
'" ,- , y" y"", , '""p~-'-"
"T", -, "' -,- ,-,",-," ,_-.-r~
r1-'-'-'-'-"r-.-_,"r -.-,_. ,_,"T""T-'-'-'-'-'-'~T-r-.-.-,..
7S ,
0a
12S ,sa ,
7S 2ae 22SINITIAL BASAL AR£A (SO FT) LEGEND:
YEAR_TRT-
j
;J
;,
;)
;)
)
j
i
j
J
,.
~j
---~---~-~--- ---.,.-
• •
2 YEAR BASAL AREA INCRtMENT
GE:OGRAPHICAL RE:GION:ONORTH IDAHO
16
e
6
B A I
o/-A
225
2ee
~
198', 2ee LBS
~
1982,CONTROL
~~
1982, 4ee Las4.
,- r-,.r-'~r-r--.-..._ ...
. ~ " • r-,-r-r""~-r'rr-"
, l "'-'-r-?'"l-r~.,...-..-.__
7S
, ."
r"~"r-'''_''''-r-r-r''''''l_''J"-..-
.lee 12S. ISe 17s ...-...., ..._
INITIAL BASAL ARE:A (sa FT)
'*-*,.
198',CONTROL
IiJ.-B-a ,
981, 41313 lBs---'-ft. '
982. 21313LBs
LtGE:ND, YE:AR_TRT
j ) ;) ) j jj j} ij j J
2 YEAR BASAL AREA INCREMENT
GEOGRAPHICAL REGION=NE OREGON
::#=
M)( = =
B A I
18
16
14
12
a
.;II
•
---e
•
r·~'1 ,-rr,-rT'rrr r','rT-,-r yy-,-r T Y'""l-r-r"'-r·TT"-'~·1-r"-'-r-""'T-r,·,-r"··"T·'-r-t"-'-'· i , , , I
75 100 125 150 175 20~ 225
INITIAL BASAL AREA esa
FT)LEGEND: YEAR TRT
• • • 1981 ~CONTROL
6 I) I) 1981 "200 LBS
o 8 e 1981"
40fa LBS
~ Q 0 1982"CONTROL
I-'I-'.. .. ..
1982, 2era LBS )( )( )( 1982" 499 LBS,...
tv
~
1981. 200Las
~
1982.CONTROL
~.1-982.
-400Las.
~
* •
~)( 4(
. 8 . . .
... 1981. CONTROL
B-a-a
1981. 400Las
---. '982, 200
Las
2 YEAR BASAL AREA INCREMENT
GEOGRAPHICAL REGI0N~CEN ~ASHINGTON
, ...,.". "-' ., ., , . "~ -" -,'''-r '-'-, -,...,.."
"-'''''''r-,-,-,.-,-,..'r' ~
-r...-"'r ... ' ,....,,..,..., _'-'-.,.7& 100 125 150 175 200 225
INITIAL BASAL AREA (SO rT)
6
81.---= _
4'f B A I
j
jJ
)
)
);
;j
J
)
i).
J j
LEGEND: YEAR_TRT
-
) }; ) ) ]) J:,\ J .) ) j j
18
2 YEAR BASAL AREA INCREMENT
GEOGRAPHICAL REGION=NE YASHINGTON
16 14
112~
. __- - - l.....---==
~ ~ . ---=-~
I 10
8
6
4 T"-"'l,"Tf"' TT f ,-,- '"r",-ry-T"·""-rTT'TT....-r-r'l'''T''-r-r'''''-'-T"'··'-r·T
,·,·,.,.,-rTTT
75
lrara125 150 175
200225
INITIAL BASAL AREA esa FT)
LEGEND: YEAR TRT • ,. • 1981, CONTROL
~ ~ ~1981 , 200 LBS
o
0 01981, 400 LBS
~ Q ~1982, CONTROL
...w.... * 1982, 2e0 LBS )( )( )( 1962, 400 LBS
;) ) ) ) ;) ) ) ) j j j
2 YEAR BASAL AREA INCREMENT
GEOGRAPHICAL REGION=MONTANA 18
'6
'4 '2
G - _ _ C
all II:
v II It
~
--,..
_ "TT
6~!"I"r _ __~
.a-- _----a
... ....e;.-.----.
--
...-~'"---
e--- ---
4 T-,-'-1-1" , -'-'-'''"r'0... ,-r -,-r ..1 , T ,-, 0' -,-.-r , ...'-1-''''-'' •-r-y- ..-rr-' -, '.--,-,·.··rr'·r'r"'''-'T
't-".,.,...
8]
B A I 1ra
75 100 125 150 175 200 225
INITIAL BASAL AREA (sa FT) LEGEND: YEAR_TRT ..-....-.. 1981; CONTROL
B-G-B
1981;
4f2J~LBS
*-*-*
1982; 200LBS
.4) 9 4
G Q Q
)( )( )(
1981;
2f2J~LBS 1982; CONTROL 1982;
4~0LBS
...
~
DES IGN r'loDEL
2
LN
(BAI) =
F ( YEAR , REGION , YEAR X REGION, INSTALLATION ( YEAR REGION)
BLOCK ( YEAR REGION INSTALLATION) TREATMENT
15
MIN
N
R2 = 0.9038
BA.x
YEARBA2
X YEARMIN
N
X TREATMENT)CV = 6.71%
) ) j ) j J J !) J ; j
18
16
2 YEAR BASAL AREA INCREMENT
GEOGRAPHICAL REGION=NE WASHINGTON
143 h---
.. 0 - - . 8 ---,-I'"t---_B ~. . >=. . . .- - -- .~"fF:-- ~
-
~Q i - I I I
Ii ~B 12}-_... . _ . _ ..
_-~---_._-:.-:-.-.- ~ ==at " " • _~
A ., ... -
*
I I0-1 .. __ -
-=-__
_ C :..,
.---_.- _. __
- 4 - - --.
=~--:
.. _ - .0 Q__ . . . - 0 - - -8-4.-·---
6
4 TT'.'-'T'"TT
'1'"
'T'r,-r'"TTrr,-rr, TO'-'TT' ,-"'0'
'-'T",,-rrrTTll , , , , 1'l-""-l"~TTrlTf"1 I , i i it 'TT'TI • I • I I II10 20 30 4Ja 50 60 70 80 90 100
MINERALIZABLE NITROGEN (PPM)
LEGEND: YEAR __ TRT
1It-1tc--.
1981 "CONTROL
~ f) ~ 1981 "200 LBS
...a-e-a
1981 .,400 LBS
G 0 4· 1962.,CONTROL
m* *
-ff- 1962.,200 LBS
K )E )E 1982.,400 LBS
;; :; ) ) ) 2J J ) iJ ) j
18
2 YEAR BASAL AREA INCREMENT
GEOGRAPHICAL REGION=CEN WASHINGTON
16-
14..:t*-- , ---*--- )( - - -
--*"----)(~------..---.---.-.- -..---... ---..
==#=-_.=tF=-~~_."• ·==tt
12t=-- ----...
- ; 3 - - . _ -====---:- .~
B -a---a---
~ ~-
A ----., _.._~--_.. ---- -~--- •. ---6-' - -~=--
: i
i:=-:::-itr
~~--~I t~l1---" _.-
_..--a---
~__
- - - O - - ". _---Itt---...---.1.-_-- ..----*
81
1..
-...-~-~----- ....---- • ----*-6~
"1",,
n n "( ' Hn "'"'I" nn~
n " " , ' " n 'IT'.r. ·r'lr r "lTnnnnrrnnn-r.,.. r· .tra
2lCl 3fa 40 5~ 60 70 8121 90 10121MINERALIZABLE NITROGEN (PPM) LEGEND: YEAR_TRT
. - . - . 1981 JCONTROL
~.. a 1981" 40121 LBS
---*_..
1982" 212J0LBS
~ ~ ~ 1961 J 200 LBS
-C-O-._+ 1962J
CONTROL
~-*""* 1 962.. 412Jf2J LBS
...
'-.I
j ) J 7 ;) ) ) ) :1 .1 j
2 YEAR BASAL AREA INCREMENT
GEOGRAPHICAL REGION=NE OREGON
18
16
14
1
12
'-. )(
._--~-_.. _-*-
>< ----.- - ..- ..--.--- tt__
·-...----·--·w ::V===
--tF=.-~ ~• ---·tt
-. --- .. _. a-- .. ---e----
"-"6---... - - - e - - - " ~ 8 -_ ~_ _.. -.()-------.-.~.-...¥--- -oil;. -"':._,
- = -i!I • r = i!Il
-1 _-_~-- Q Q - • --*-ie-.. - ~---.-
-i .---~.,....- - -
6] .--.--. -
- ...---
-JIt---""*---4 .
r"r,r " ' r T lrrrTT" .. r r ,
rr
r .. , 'T' , 'T'-'·'.... ,...·'TTTTrr·n ...,.l'·r ,."." "'TTTrrr.,. TTrTrrrn...-rrTrT.,...I I I I rB
A I 10
10
2ra 3ra
40 50sra
708ra
90lrara
MINERALIZABLE NITROGEN (PPM)
LEGEND: YEAR_TRT
.~-..1981.. CONTROL
~ ~..
~1981 .. 2rara LBS
...&-B--f}
1981.. 4f2J0 LBS
Q Q ~1982 .. CONTROL
co*-*-* 1982 .. 200 LBS )( )( )( 1982.. 40ra LBS
;> J ) ;) j ) )
j ) j J
18
16 14
2 YEAR BASAL AREA INCREMENT
GEOGRAPHICAL REGION=CENTRAL IDAHO
--- )( - ) ( )(
._"""-*~---12i1r--. _-- - -._---tt--- 4t__--- ----
* 1t==::::=:::w=-
--¥- II = Jt B:r--
B- - a - - - -
0 - - f 8 = t - - - -A
r---~-- -- ~ . -~_. i
:ij"==- 8 .~_o-,...---' - ' f j 8==~
I 1fa Q 0 : :
=-_ *_--~---*
~ 0 31& - - ,..
1 .-
1 ! - - - ~-10 20 30 40 5fa 60 70 80 90 100
MINERALIZABLE NITROGEN (PPM)
LEGEND: YEAR_TRT ..-.... - .. t98 t" CONTROL ~ ~ _.~ 1981 ~ 200 LBS ...
&-B--f.} t 981" 400 LBS ~ • -.Q. 1982" CONTROL \D
~-.. 1982~ 200 LBS )( )( )( 1982~ 400 LBS
:; ) ;) ) } } ) j
:} j j
18
2 YEAR BASAL AREA INCREMENT
GEOGRAPHICAL REGION=MONTANA
16
14
t
2 -f BA
I :b- ..
-6--_. - B - - - 6 - - - __~ ~ i : _._
II " . - ,~
t
0r-f:"-_
-/T--_ <> .- ·.h. "~
-- ...
.t. ~
.I. _ - - - -
'
.---
~ ~
8-1 .... __- - - ..
_----..or.- -4?--.
*= ¥ = = " ..
.M'-- --. )t-:-.=...~ . ... -:-0_. -_ . •_~-----'-'. ...w-=- __:::::_.:=: ...:..: ..._ ~
.JII -~=---.===-.0°·.· tt---.. -'"W----_o. - .
6
00--
~---"-.-.-
- -...- - - 0---0--.---<>---- _ ...- - -~
_ _.o_e
4 , J"' ,,r, " '1"1"11
'0' ,
,o,r" r-IT11"O'O'Tr'r," ' T I"l-rrTlT'Tn-r,-r,"-"" T-TT,T T l ' r r,o.-" .. ,rrr,,,,,,orl • I , ,ITTTJ1ra 2ra 3ra
40 50sra
7ta 80 9ta tta0MINERALIZABLE NITROGEN (PPM) LEGEND: YEAR_TkT
--~-.t981
JCONTROL
a-a-·-e
1981
J 40taLBS
• .# -* 1982J
200 LBS
+-~-~ I 98 1J
200 LBS
4-~~ 1982J
CONTROL
W v~ t982~
400 LBS
I\.)
o
) :; )I
) ) } )
) ) ) J
2 YEAR BASAL AREA INCREMENT
GEOGRAPHICAL REGION=NORTH IDAHO
\0 20 30 40 60 60
70 80 9ltl 1ltl0
MINERALIZABLE NITROGEN CPPM)
LEGEND: YEAR_1RT ~ • • 198\J CONTROL +
e
~ '96\J 200 LBS IVa--e---9 \
98' J 400 LBS..cr Q ~ '982 .. CONTROL ~
.-._*
'982 .. 200 LBS*
X*
\962 .. 400 LBS_...---
_--4---
e----'- ______
. ..---....--
~
:1 41
1
n'" n , n Inn ...._.,., Tn,., ,-., , ' p n , ",.
-nrn-
n "'''''T'-n ....n",-n-rrrrn-rp ,...n"'-' • • , rrTTTt-nTB
A I \0
) ) .> ;) .) ) :1 ") ;) .I J
2 YEAR BASAL AREA INCREMENT
GEOGRAPHICAL REGION=NE UASHINGTON
18
16
• __:t
~
r1
'OJ -
---a--- --
~
..
e---
r----
8
I'll
12
J
~ ~
I 10 6)
J
.)
)
;)
j)
)
j
tv t.J j )
)
>( - - k
if •
~
1981. 200lBS
~
1982. CONTROL~
1982. 400 lBs~ ....---
~
'I< '98'. CONTROLB--£J--fJ , 9£$/.
400lBs
*--.--.
1982. 200 lBS2 YEAR BASAL AREA INCREMENT
GeOGRAPHICAL ReGION~ceN WASHINGTON
---*
- - #
18
-4,
"IT-r"l-r-.,..,. ,. r,·r""r"r r r" _
, , , , T ,-..-, "-'-"'-,,_""-"-r-,.". ,."_'-' -".. ,-,.,_, ...-, , _,_...-,.,-
75 I 00 , 25 , S0 I 75 200 22S
INITIAL BASAL AReA (SQ FT)
B A I
LEGEND: YEAR_TRT
-
) :; }) :) ) ) -; ) .] 3 j
18
16
14
12 B A I
1ta
8
6---..-
4
2 YEAR BASAL AREA INCREMENT
GEOGRAPHICAL REGION=NE OREGON
~ = ~ = - ..
• * *
ale
r-r'-rT-TI"~-rl-r,. r T T ' " "'-TTr'.,.·'·l·.-r-T.,....TTr~TI·T-'-rTl'-TrT.,·r-l-r" .,-,-• • • • • • • I
75
10ta .125 150 176 200
225INITIAL BASAL AREA (sa FT)
LEGEND: YEAR TRT * •• 1981
JCONTROL
~ $ ~ t98t~200 LBS
IVa-e-a 1981
J400 LBS
c; Q II t982~CONTROL
~* •. *
1982J 200 LBS)( )( )(
1982~400 LBS
") ) ") ) ;) ) ) ) ) ') }
2 YEAR BASAL AREA INCREMENT
GEOGRAPHICAL REGION=CENTRAL IDAHO
16
1
116
14 -K
)(
:: ..
~
--- ..
8
6
--e--
A.~_ _
---_Q.o---= •
III*
---
) ) ) i) j j :; ) ) }) }
18
16
14
~
121
I
101
8
6
4
2 YEAR BASAL AREA INCREMENT
GEOGRAPHICAL REGION=MONTANA
- _--= ~ ;; ;;;; :: :=I
=it:
;<;?"-~-
-. . . - Q Q Q _.--~
r~r·fO-T,-rrrT r-r-r"T-rrr-J-rT,,-r Of I I I
,-r-r-t.,-r'-'-rr
I I I'-T--r-T",.-.-'
I I I I I I I J75
100 125 150 175 20121
225INITIAL BASAL AREA (sa FT)
LEGEND: YEAR_TRT
.-~-.1981
JCONTROL
~ & & 1981 12121121 LBS
I\)e 8 8 1981 J
412J12J LBS
-c- Q •1982 .. CONTROL
0'\* • * 1982.. 20121 LBS )( )( )( 1982.. 4121121 LBS
) ) ;) ) j) }) ) ) 1 ) j
2 YEAR BASAL AREA INCREMENT
GEOGRAPHICAL
REGION=NORTH
IDAHO6 8 16
~
...
.. ...
14
12 18
B
A
I 1~~
4 r...r-T·r'·' ..."-r'-Y,l-r.,-r-y--r.-rr,--r-' '-T-r-TTr-r"'rrT"T ...rT' ' r 'I'r'-'-T-'-rr"'-'-' i i i , I
75 1f2Jf2J 125 t5~ 176 200 225
INITIAL BASAL AREA (sa FT)
LEGEND:
YEAR_TRT . . - . - . 1981 " CONTROL ~ ~ ~ 1981 ~ 200 LBS N8 8 8 I 981 " 4~ra
LBS
Q Q ca 1982"CONTROL
-..J... -- 1982" 200 LBS )( )(~ 1962" 400 LBS
28
Jim Moore
Department of Forest Resources University of Idaho
Predictive Model of Response to Nitrogen Fertilization
~ Contrast with design model
=
differences between installations rather than within installations.Predictive model R2 = .70 vs. R2 = .90 for the Design Models.
Variables in the predictive model that account for underlying
~ differences in growth between installations but do not interact with treatment are:
*S01l Depth - deep soils (>24") grow better than medium (12 to 24 " ) grow better than shallow soils (~12").
*Ash Depth - (where present) deep better than shallow ash illustrated later.
ash soils (>12") grow caps. This will be
of Figures illustrates the relationships growth response and initial basal area by
Figure 4.
*Douglas-fir site index (Monserud 1984) as site index increases growth increases. See Figure 1.
*Slope and aspect this is expressed as an interaction term (Stage 1976) in the model. The highest basal area increment occurs on Southerly aspects (other factors being equal). Similar results from other studies in Northern Hemisphere. See Figure 2.
*Soil parent material and initial stand density (basal area) - also influence the underlying differences in basal area growth rate between installations.
But more importantly they significantly interact with treatment. They both are important in predicting treatment response.
The next series between treatment parent material.
Figure 3. A bar graph showing differences in relative (%) response to treatment by parent materials.
Note: No response for valley fills and very large % response for sandstone.
The effect of initial basal area on relative response for Ash/Metasediments.
Notes: (1) This parent material is confined to North Idaho.
29
(2) (3) (4)
Relative response is highest at low densities.
The 400 lb. treatment is significantly more than the 200 lb. treatment.
Thi 30% response line. For2200 Ibs.
=
117Ft lAc.; for 400 Ibs.
=
204 Ft lAc.Figure 5. The effect of initial basal area on relative response for basalts.
the
Notes: (1)
(2)
Relative response is highest at low stand densities.
There is no significant difference between 200 and 400 lb. treatments.
Figure 6. The effect of initial basal area on relative response for granite.
(1) (2)
Notes: Relative response is highest at low stand density.
There is no significant difference between the 200 and 400 lb. treatments.
Figure 7. The effect of initial basal area on relative response for Valley fill.
Notes: (1) This parent material was sampled only in Montana.
(2) There was no treatment response on this parent material.
Figure 8. The effect of initial basal area on relative response for colluvium.
...,
(3)
(1) (2)
Notes: This parent material was sampled only in Montana.
There was a significant difference between the 200 and 400 lb. treatments.
There was a very high % response on this parent material, but this may not translate to as much absolute basal area response depending on the level of untreated growth.
This will be illustrated in SUbsequent figures.
Figure 9. The effect of initial basal area on absolute basal area increment for ash/metasediments with shallow ash (~12U).
Notes: (1) Control 2-year basa~ area increment peaks at approximately 130 Ft lAc.
(2) Absolute basal area response for the 200 lb.
treatment is highest at the lowest stand
30
densities, but the curve is relatively flat over the range of densities sampled.
(3) Absolute response f0
2
the 400 lb. treatment peaks at about 120 Ft AC., although resionse is predicted to be greater than 4 F~ /Ac.even at an initial basal area of 175 Ft . (4) Ash/metasediment soils were sampled only in
North Idaho.
Fiqure 10. The effect of initial basal area on absolute basal area increment for ash/metasediments with deep ash
(~121')•
Notes: (1) The contrast of this fiqure with fiqure 9 illustrates the effect of having a deep ash cap on the site. There is an increase in the amount of absolute response to treatment due to the higher baseline (normal) growth on deep ash soils.
Fiqure 11. The effect of initial basal area on absolute basal area increment for ash/loess with a deep ash
(~12")• (1)
(2) (3)
Notes: Control (untreated) gro~h peaks at an initial basal area of 200 Ft /Ac.
Treatment response peaks at about 170 Ft2/AC.
There is no significant difference between the 200 and 400 lb. treatments.
Fiqure 12. The effect of initial basal area on absolute basal area increment for glacial t i l l with deep ash.
Notes: (1)
(2) (3) (4)
co~trol (untreated) qrowth peaks at about 160 Ft /Ac. initial basal area.
Response to the 200 lb. treatment is h~qhest
at the lowest initial basal area (75 Ft lAc).
Absolute response to thi 400 lb. treatment is largest at about 100 Ft initial basal area.
The response curves are relatively flat over the range of basal areas sampled on this parent material.
Fiqure 13. The effect of initial basal area on absolute basal area increment for granite.
Notes: (1)
(2)
Control growth is greates~ at an initial basal area of about 160 Ft for this parent material.
Absolute basal area response to the 200 lb.
treatment is qriatest at the lowest initial basal area (75 Ft lAc.).
31
(3) Response to the 400 lb. treatment peaks at an
in~tial basal area of approximately 125
Ft lAc.
(4) The response curves are relatively flat over the range of basal areas sampled. Similar to the pattern shown for glacial tills.
Figure 14. The effect of initial basal area on absolute basal area increment for colluvium.
Notes: (1) Because of the very slow normal (untreated) growth on this parent material, the "huge"
percent response (shown in Figure 8) translates to only a "large" absolute response.
(2) A relatively narrow range of initial basal area was sample2 on this parent material
( 105 to 175 Ft lAC.) and the curves do not extrapolate well outside of this basal area range.
(3) This parent material was sampled only in Montana.
Figure 15. The effect of initial basal area on absolute basal - area increment for alluvium.
Notes: (1) Control (untreated) growth pe2ks at an initial basal area of about 170 Ft lAc.
(2) Absolute basal area response to the 200 lb.
treatment is greatest
2at an initial basal of approximately 160 Ft lAc. for both nitrogen treatments.
(3) The response to the 400 lb. treatment is less than for the 200 lb. treatment on this parent material. SUbsequently, we discovered that the plots for the 400 lb. treatments had higher pre-treatment nitrogen mineralization rates (Min-N) than the 200 lb. treatment plots. When we statistically adjust for the differences in pre-treatment Min-N, the response to 400 lbs. becomes slightly higher than for the 200 lbs. treatment.
) ) ~ ) ") ) ~J j y J )
2 YEAR BASAL AREA INCREMENT
GLACIAL
TILL~12- OR LESS
ASH~AVERAGE SOIL DEPTH
8Aa150~ SLOPEa2S~
ASPECTal80
• • • I • • • • • I ~""'-"T.
. . . .
I • • • • • • • • • I • • • • • • e I • I • , • • • • • • • ISITE INDEX (FEET AT 50 YEARS) B
A I
49 60 60 70
80
90100
wt\)
Eigure 1. The relationship between untreated two-year basal area increment per acre and Douglas-fir site index.
;> ) ) ;; j) ) .J j } .>
,
2 YEAR BASAL AREA INCREMENT
GLACIAL
TILL~ 12-OR LESS
ASH~AVERAGE SOIL DEPTH
BA=t60~
SITE INDEX=70
B A I
10.0 9.8
• • • • I • • • • • • • • • I • .,T. • • • • I • • • • • • • • • I
9 4S 99 ISS t89 22S 279' SIS 369
ASPECT (DEGREES) LEGEND- SLOPE
• • • 19 "• • • 49 "
• • • 20 "At Ia At S0 "
a a a
30 "w: w:
Nt60 "
wwFigure 2. The relationship between untreated two-year basal area increment per acre and slope and aspect.
BAI INCREASE OVER CONTROL (%)
BY TREATHENT AND PARENT HATERIAL .
.:;. • J .3 ;; j j J J' ) ) :»
RESPOOSE 188
Fie
8 I I ' "
"1'
" I I . .-58
2 .. 2 .. 2 .. 2 .. 2 • 2 .. 2 • 2 4 2 ..
e
8 8e
8e e
8 8 8e
8 8e e e e
8 TRTHENT8 8 8 8 (I 8 8 8 (I 8 8 8 8 8 8 8 8 8
G
A
IS TA F
CA S
R S A
IS
I 0 LA
A
HS
LH
L L L NN
IA
L / L L U 0 P_HATERL
LH U V
T V
w
Figure 3. Two-year relative basal area response by soil parent material. ~
) ) , ) ;) p iJ ~ ) ; ;) J
BAI INCREASE DUE TO FERTILIZATION
PARENT MATERIAL-ASH/METASEDIHENT
P
E R
C E
N T
o
F
I
75 lea
125 159 175 28a225
INITIAL BASAL AREA (SO FT)
LEGEND. TRTHENT • • • CONTROL
~ A •298 LBS o
II []-489 LBS
wU1
Figure 4. The effect of initial basal area on relative response for Ash/Metasediments.
) , j ) ;) ) J!J ) J j . ) )
SAl INCREASE DUE TO FERTILIZATION
PARENT HATERIALaBASALT
c o
N
T R
O . I . I
L
~
I ,-10 i • i • • i • i • • ••••••••• 1•••••••••••••••• 1•••••••••••••••••••••••••
o
FP E _
R 79 C
E N
T
75 190 125 158 175 290 225
INITIAL BASAL AREA
(SaFlY
LEGEND. JRTHENT • • • CONTROL
~ A A 299 LBS [I 9 B 499 LBS Yigure 5. The effect of initial basal area on relative response for Basalt.W 0\
) :J i"'-I j ) 21 .) w ;) ') J
BAI INCREASE DUE TO FERTILIZATION
PARENT MATERIAL-GRANITE
o
f
3_ I
C I
~
IT 19 I I
R I
o
J . . .. tit I • • •L
II
-19 I
P E
R
C
E
N
T
15 109
125159 175 299 225
INITIAL BASAL AREA (sa FT)
LEGEND- TRTHENT
.. .. litCONTROL
.. A A299 LBS
[] [J Il400 LBS
Figure 6. The effect of initial basal area on relative response for granite.
w~
; ;) )J } . ) 11 i) 11 ) ;>
}
BAI INCREASE DUE TO FERTILIZATION
PARENT MATERIAL-VALLEY FILL
.p E
R
C
E N T
o F
o
C NT 1
R o
L
10 ••••••••• ' ••
'1.'
... Ii • • • • • i i i i I • • • • • • • • 1 • • • • • • • ' • • • • 1 • • • • • • • • • • • •
75
199 125 159 175 290 225INITIAL BASAL AREA (Sa FT)
LEGEND- TRTHENT
III • IIICONTROL
~ ~ ~ 299 LBS D [) D 499 LBSw
00
Yigure 7. The effect of initial basal area on relative response for valley fill.
) ;) )J j J j ;) j :; .> j)
BAI INCREASE DUE TO FERTILIZATION
PARENT MATERIAL-COLLUVIUM
o F
C
o
N
T I
R
o
L ...1U " . i i i • • • • • •f t i • i • i i • • • • • • • • • • • • • • • • • • • • • "
P E
R C E
N T
75 10a 125 168 176 299 225
INITIAL BASAL AREA (SO FT)
LEGt:ND. TRTHENT .. • • CONTROL
.. A A 299 LBS 9 g B 499 LBSW
\0
Vigure 8. The effect of initial basal area on relative response for colluvium.
; J )... ) ;) J )J } j 11 ~
-- "
2 YEAR BASAL AREA INCREMENT·
PARENT MATERIAL-ASH/METASEDIMENT ASH CAP DEPTH=12- OR LESS 22
28 18
B 12
1 . . .
~A . •
I to •
76 tee
t25 t60 1762ee
225INITIAL BASAL AREA (sa FT)
LEGEND. TRTMENT .. .. .. CONTROL • • • 2ga LBS
B B B4ga LBS
~o
~Figure 9. The effect of initial basal area on absolute basal area increment for ash/
metasediments with shallow ash (~l2n).
) -} ;; J ) :a ) ;) .1 ), t
2 YEAR BASAL AREA INCREMENT
PARENT HATERIALaASH/HETASEDIMENT ASH CAP DEPTH=HORE THAN 12-
22 29
B
A
J:76 100 125 160 176 .' 200 225
INITIAL BASAL AREA (sa FT)
LEGEND
ITRTHENT • • • CONTROL
• e • 290LBS
B B B 400LBS
oI:lo f-4
Figure 10. The effect of initial basal area on absolute basal area increment for ash/metasediments with deep ash (>12").
j ;; figure 11. JThe effect of i'tltlol basot ord} on absolute bLtal or.o Increa..Jt for osh/loeS8 l.fth deeposh (,.211) .
2 YEAR BASAL AREA INCREMENT
PARENT HATERIALaASH/LOESS ASH CAP DEPTH=MORE THAN 12-
J; y
76 199 0125
169 176 o.290 225
INITIAL BASAL AREA (SO
FT)LEGEND
ITRTHENT ... • CONTROL
• • • 290LBS
Il B B -490LBS
os:.
to.)
Figure 11. The effect of initial basal area.on absolute basal area increment for ash/
loess with deep ash (>12").
) ::i ) ~ J J ) j ) ~ ":\.~
2 YEAR BASAL AREA INCREMENT
PARENT MATERIAL-GLACIAL TILL ASH CAP DEPTH=MORE THAN
12-76 t99
125169 176 ". 299
225INITIAL BASAL AREA (SO FT)
LEGEND. TRTHENT .. .. .. CONTROL
• A A 2ra9LBS
Il B B -49aLBS
.a:.w
Figure 12. The effect of initial basal area on absolute basal area increment fo~
glacial till with deep ash.
;; j ) :J ) .} ) ) ) ~ J
2 YEAR BASAL AREA INCREMENT
PARENT MATERIAL-GRANITE ASH CAP DEPTH=12- OR LESS
76 100 126
159 175200
225INITIAL BASAL AREA (sa FT)
~i9ure 13. The effect of initial basal area on absolute basal area increment for granite.
LEGEND
aTRTMENT • • • CONTROL
• e e2sa LBS
B B B-4aa LBS
~
~
) j ) J ;) J ) j ) } }
2 YEAR BASAL AREA INCREMENT
PARENT MATERIALaCOLLUVIUH ASH CAP DEPTH=12- OR LESS
29
76
IB8 125 IS0176 . 208
225INITIAL BASAL AREA (SO FT)
Fiqure 14. The effect of initial basal area on absolute basal area increment f0r colluvium.
LEGEND
ITRTHENT
III III IIICONTROL
• • • 209LBS
B B B -409LBS
~
U1
) j ) .ll ;; ) ) J J 3' )
22 28
2 YEAR BASAL AREA INCREMENT
PARENT HATERIALaALLUVIUM ASH CAP DEPTH=12- OR LESS
I. i i i i i i i , , i i i i , , • • • i i ' i i ' • • , • • • • • • • , • , , • , , " • • • • • • I • • • • • • • • • I
76
t00 t25 15e 176.. 299
225INITIAL BASAL AREA (sa FT)
Figure 15. The effect of initial basal area on absolute basal area increment for alluvium.
LEGEND- TRTHENT • • • CONTROL • • • 2ae LBS
B B B480 LBS
.e:..
0'\
47
Summary
What have we gained in a practical sense from the information just presented? One way to illustrate the gains from the new information is to go through the following scenarios:
If we had applied 200 lbs. of nitrogen per acre to all the managed Douglas-fir stands in the Intermountain region as represented by our installations, we would have obtained
th~ overall average 2-year basal area response of 2.4 Ft lAc. or an average 31% increase in basal area growth.
These numbers are probably higher than we expected at the beginning of the project. But if these are th$ averages, think what response we must be getting on the best responders!
Table 1 illustrates how we can use the predictive models to eliminate the non-responders and concentrate the treatments on the better responding sites. Each contrast represents conditions that are common in each region (not the best or worst). The comparisons were selected to show the effects of parent materials and stand density on response in a useable way.
These differences will determine the profitability of an operational fertilization program if they continue in the same manner over time.
The evidence to date certainly indicates that nitrogen fertilization should be strongly considered as a viable silvicultural treatment on many sites in the Intermountain West. The key is to identify the best responding sites and concentrate on those that produce the highest return on the investment. We have come a long way toward identifying those sites in the last several years.
Table 1. Predicted response to 200 pounds of nitrogen per acre for various site and stand conditions in each geographi.c region.
GROWTH RESPONSE TO 200 LB. N/Ac.
48
SA/Aci PERCENT
OVERALL 2.4 31
~
ASH/METASEDIMENTS 5.7
liDGLACIAL TILL 118 20
Mc.mM
COLL.UVIUM 3.7 65
VALLEY FILL. -0.5 - 8
~
BASALT 316
~2GRANITE 1.2 16
,.,..~OBJijEAST
OREGON
ASH/LoESS 315 33
BASAL.T 119 22
CENIRAL WASHINGTON
·SANDSTONE 616 71
BASALT 316 42
GLACIAL TILL. 1.8 20
MORTHEAST WASHINGTON
GLACIAL TIL.L 3.7 39
BASALT
,.,..