Variation in green density and moisture content of radiata pine trees in the Hume region of New South Wales

SummaryVariation in green density and moisture content are relevant for log transport planning, weight-scaling systems, lumber drying and dynamic assessment of stiffness. The lack of published Australian reports on the subject prompted the present study (most studies with radiata pine have been carr...

Full description

Saved in:
Bibliographic Details
Published inAustralian forestry Vol. 75; no. 1; pp. 31 - 42
Main Authors Chan, Julian Moreno, Walker, J. C.F, Raymond, C. A
Format Journal Article
LanguageEnglish
Published Taylor & Francis Group 2012
Subjects
Online AccessGet full text
ISSN2325-6087
0004-9158
2325-6087
DOI10.1080/00049158.2012.10676383

Cover

Abstract SummaryVariation in green density and moisture content are relevant for log transport planning, weight-scaling systems, lumber drying and dynamic assessment of stiffness. The lack of published Australian reports on the subject prompted the present study (most studies with radiata pine have been carried out in New Zealand).Patterns of variation in green density and moisture content of radiata pine as influenced by age, site, thinning regime, height in the stem and season were investigated using paired stands of mature trees (34.5–36.5 y old) on contrasting sites and with various thinning regimes, and a stand of young trees (9 y old), in the Hume region of New South Wales. Destructive samples were taken from mature trees at successive heights in the stem, and from young trees at 1.3 m. The effect of extended drought was included by using data from separate studies. The effect of green density variation on weight scaling was determined by calculating weight-to-volume conversions for a number of stands under two climatic scenarios.Under normal climate, sapwood green density averaged about 1100 kg m⁻³ and showed little variation across ages, seasons, sites, thinning regimes and height in the stem. Sapwood saturation showed small but consistent differences with age, season and height in the stem, but practically no differences with site and thinning regime. For mature trees, sapwood saturation ranged from 90% at the base of the tree to 92–94% higher up in the stem, whereas for young trees it averaged 96% at 1.3 m height.Heartwood green density varied greatly with height in the stem, but showed no consistent differences with site and thinning regime; it ranged from about 550 to 630 kg m⁻³ at 1.3 m height across mature stands. Heartwood saturation averaged about 7% at 1.3 m, decreased from the base of the tree to 10.5 m followed by an increase up the stem, was higher in the high-altitude site and decreased slightly from winter to summer.Whole-section green density was driven by the ratio of sapwood to heartwood that in turn was affected primarily by age and height in the stem, followed by site and to a lesser extent by thinning regime. Season exerted practically no effect on whole-section green density. Whole-section green density varied-considerably between mature stands, ranging from 943 to 1023 kg m⁻³ at 1.3 m height, 928 to 996 kg m⁻³ at 10.5 m, and 960 to 1016 kg m⁻³ at 16 m.Whole-section green density and thus weight-to-volume conversions were significantly affected by site, age and severe drought, but not by thinning regime nor season. Using a common conversion factor between contrasting sites would lead to errors of 3–5%). The errors in applying such a factor to unthinned stands under severe drought would be 10% (large trees), 12% (average trees) and 25% (suppressed trees). The errors for the 9–10.5-y-old trees under normal climate would be 8–10% and up to 5% under severe drought. If a separate conversion factor was set for young trees, conversions under severe drought would have an error of 9–13%. It is then advisable to determine variations in green density at site and age levels in large plantation areas with a range of growing conditions and age classes, as well as to monitor changes during extended droughts.
AbstractList Variation in green density and moisture content are relevant for log transport planning, weight-scaling systems, lumber drying and dynamic assessment of stiffness. The lack of published Australian reports on the subject prompted the present study (most studies with radiata pine have been carried out in New Zealand). Patterns of variation in green density and moisture content of radiata pine as influenced by age, site, thinning regime, height in the stem and season were investigated using paired stands of mature trees (34.5-36.5 y old) on contrasting sites and with various thinning regimes, and a stand of young trees (9 y old), in the Hume region of New South Wales. Destructive samples were taken from mature trees at successive heights in the stem, and from young trees at 1.3 m. The effect of extended drought was included by using data from separate studies. The effect of green density variation on weight scaling was determined by calculating weight-to-volume conversions for a number of stands under two climatic scenarios. Under normal climate, sapwood green density averaged about 1100 kg m −3 and showed little variation across ages, seasons, sites, thinning regimes and height in the stem. Sapwood saturation showed small but consistent differences with age, season and height in the stem, but practically no differences with site and thinning regime. For mature trees, sapwood saturation ranged from 90% at the base of the tree to 92-94% higher up in the stem, whereas for young trees it averaged 96% at 1.3 m height. Heartwood green density varied greatly with height in the stem, but showed no consistent differences with site and thinning regime; it ranged from about 550 to 630 kg m −3 at 1.3 m height across mature stands. Heartwood saturation averaged about 7% at 1.3 m, decreased from the base of the tree to 10.5 m followed by an increase up the stem, was higher in the high-altitude site and decreased slightly from winter to summer. Whole-section green density was driven by the ratio of sapwood to heartwood that in turn was affected primarily by age and height in the stem, followed by site and to a lesser extent by thinning regime. Season exerted practically no effect on whole-section green density. Whole-section green density varied-considerably between mature stands, ranging from 943 to 1023 kg m −3 at 1.3 m height, 928 to 996 kg m −3 at 10.5 m, and 960 to 1016 kg m −3 at 16 m. Whole-section green density and thus weight-to-volume conversions were significantly affected by site, age and severe drought, but not by thinning regime nor season. Using a common conversion factor between contrasting sites would lead to errors of 3-5%). The errors in applying such a factor to unthinned stands under severe drought would be 10% (large trees), 12% (average trees) and 25% (suppressed trees). The errors for the 9-10.5-y-old trees under normal climate would be 8-10% and up to 5% under severe drought. If a separate conversion factor was set for young trees, conversions under severe drought would have an error of 9-13%. It is then advisable to determine variations in green density at site and age levels in large plantation areas with a range of growing conditions and age classes, as well as to monitor changes during extended droughts.
Variation in green density and moisture content are relevant for log transport planning, weight-scaling systems, lumber drying and dynamic assessment of stiffness. The lack of published Australian reports on the subject prompted the present study (most studies with radiata pine have been carried out in New Zealand). Patterns of variation in green density and moisture content of radiata pine as influenced by age, site, thinning regime, height in the stem and season were investigated using paired stands of mature trees (34.5–36.5 y old) on contrasting sites and with various thinning regimes, and a stand of young trees (9 y old), in the Hume region of New South Wales. Destructive samples were taken from mature trees at successive heights in the stem, and from young trees at 1.3 m. The effect of extended drought was included by using data from separate studies. The effect of green density variation on weight scaling was determined by calculating weight-to-volume conversions for a number of stands under two climatic scenarios. Under normal climate, sapwood green density averaged about 1100 kg m⁻³ and showed little variation across ages, seasons, sites, thinning regimes and height in the stem. Sapwood saturation showed small but consistent differences with age, season and height in the stem, but practically no differences with site and thinning regime. For mature trees, sapwood saturation ranged from 90% at the base of the tree to 92–94% higher up in the stem, whereas for young trees it averaged 96% at 1.3 m height. Heartwood green density varied greatly with height in the stem, but showed no consistent differences with site and thinning regime; it ranged from about 550 to 630 kg m⁻³ at 1.3 m height across mature stands. Heartwood saturation averaged about 7% at 1.3 m, decreased from the base of the tree to 10.5 m followed by an increase up the stem, was higher in the high-altitude site and decreased slightly from winter to summer. Whole-section green density was driven by the ratio of sapwood to heartwood that in turn was affected primarily by age and height in the stem, followed by site and to a lesser extent by thinning regime. Season exerted practically no effect on whole-section green density. Whole-section green density varied-considerably between mature stands, ranging from 943 to 1023 kg m⁻³ at 1.3 m height, 928 to 996 kg m⁻³ at 10.5 m, and 960 to 1016 kg m⁻³ at 16 m. Whole-section green density and thus weight-to-volume conversions were significantly affected by site, age and severe drought, but not by thinning regime nor season. Using a common conversion factor between contrasting sites would lead to errors of 3–5%). The errors in applying such a factor to unthinned stands under severe drought would be 10% (large trees), 12% (average trees) and 25% (suppressed trees). The errors for the 9–10.5-y-old trees under normal climate would be 8–10% and up to 5% under severe drought. If a separate conversion factor was set for young trees, conversions under severe drought would have an error of 9–13%. It is then advisable to determine variations in green density at site and age levels in large plantation areas with a range of growing conditions and age classes, as well as to monitor changes during extended droughts.
SummaryVariation in green density and moisture content are relevant for log transport planning, weight-scaling systems, lumber drying and dynamic assessment of stiffness. The lack of published Australian reports on the subject prompted the present study (most studies with radiata pine have been carried out in New Zealand).Patterns of variation in green density and moisture content of radiata pine as influenced by age, site, thinning regime, height in the stem and season were investigated using paired stands of mature trees (34.5–36.5 y old) on contrasting sites and with various thinning regimes, and a stand of young trees (9 y old), in the Hume region of New South Wales. Destructive samples were taken from mature trees at successive heights in the stem, and from young trees at 1.3 m. The effect of extended drought was included by using data from separate studies. The effect of green density variation on weight scaling was determined by calculating weight-to-volume conversions for a number of stands under two climatic scenarios.Under normal climate, sapwood green density averaged about 1100 kg m⁻³ and showed little variation across ages, seasons, sites, thinning regimes and height in the stem. Sapwood saturation showed small but consistent differences with age, season and height in the stem, but practically no differences with site and thinning regime. For mature trees, sapwood saturation ranged from 90% at the base of the tree to 92–94% higher up in the stem, whereas for young trees it averaged 96% at 1.3 m height.Heartwood green density varied greatly with height in the stem, but showed no consistent differences with site and thinning regime; it ranged from about 550 to 630 kg m⁻³ at 1.3 m height across mature stands. Heartwood saturation averaged about 7% at 1.3 m, decreased from the base of the tree to 10.5 m followed by an increase up the stem, was higher in the high-altitude site and decreased slightly from winter to summer.Whole-section green density was driven by the ratio of sapwood to heartwood that in turn was affected primarily by age and height in the stem, followed by site and to a lesser extent by thinning regime. Season exerted practically no effect on whole-section green density. Whole-section green density varied-considerably between mature stands, ranging from 943 to 1023 kg m⁻³ at 1.3 m height, 928 to 996 kg m⁻³ at 10.5 m, and 960 to 1016 kg m⁻³ at 16 m.Whole-section green density and thus weight-to-volume conversions were significantly affected by site, age and severe drought, but not by thinning regime nor season. Using a common conversion factor between contrasting sites would lead to errors of 3–5%). The errors in applying such a factor to unthinned stands under severe drought would be 10% (large trees), 12% (average trees) and 25% (suppressed trees). The errors for the 9–10.5-y-old trees under normal climate would be 8–10% and up to 5% under severe drought. If a separate conversion factor was set for young trees, conversions under severe drought would have an error of 9–13%. It is then advisable to determine variations in green density at site and age levels in large plantation areas with a range of growing conditions and age classes, as well as to monitor changes during extended droughts.
Summary Variation in green density and moisture content are relevant for log transport planning, weight-scaling systems, lumber drying and dynamic assessment of stiffness. The lack of published Australian reports on the subject prompted the present study (most studies with radiata pine have been carried out in New Zealand).Patterns of variation in green density and moisture content of radiata pine as influenced by age, site, thinning regime, height in the stem and season were investigated using paired stands of mature trees (34.5–36.5 y old) on contrasting sites and with various thinning regimes, and a stand of young trees (9 y old), in the Hume region of New South Wales. Destructive samples were taken from mature trees at successive heights in the stem, and from young trees at 1.3 m. The effect of extended drought was included by using data from separate studies. The effect of green density variation on weight scaling was determined by calculating weight-to-volume conversions for a number of stands under two climatic scenarios.Under normal climate, sapwood green density averaged about 1100 kg m⁻³ and showed little variation across ages, seasons, sites, thinning regimes and height in the stem. Sapwood saturation showed small but consistent differences with age, season and height in the stem, but practically no differences with site and thinning regime. For mature trees, sapwood saturation ranged from 90% at the base of the tree to 92–94% higher up in the stem, whereas for young trees it averaged 96% at 1.3 m height.Heartwood green density varied greatly with height in the stem, but showed no consistent differences with site and thinning regime; it ranged from about 550 to 630 kg m⁻³ at 1.3 m height across mature stands. Heartwood saturation averaged about 7% at 1.3 m, decreased from the base of the tree to 10.5 m followed by an increase up the stem, was higher in the high-altitude site and decreased slightly from winter to summer.Whole-section green density was driven by the ratio of sapwood to heartwood that in turn was affected primarily by age and height in the stem, followed by site and to a lesser extent by thinning regime. Season exerted practically no effect on whole-section green density. Whole-section green density varied-considerably between mature stands, ranging from 943 to 1023 kg m⁻³ at 1.3 m height, 928 to 996 kg m⁻³ at 10.5 m, and 960 to 1016 kg m⁻³ at 16 m.Whole-section green density and thus weight-to-volume conversions were significantly affected by site, age and severe drought, but not by thinning regime nor season. Using a common conversion factor between contrasting sites would lead to errors of 3–5%). The errors in applying such a factor to unthinned stands under severe drought would be 10% (large trees), 12% (average trees) and 25% (suppressed trees). The errors for the 9–10.5-y-old trees under normal climate would be 8–10% and up to 5% under severe drought. If a separate conversion factor was set for young trees, conversions under severe drought would have an error of 9–13%. It is then advisable to determine variations in green density at site and age levels in large plantation areas with a range of growing conditions and age classes, as well as to monitor changes during extended droughts.
Author Chan, Julian Moreno
Walker, J. C.F
Raymond, C. A
Author_xml – sequence: 1
  fullname: Chan, Julian Moreno
– sequence: 2
  fullname: Walker, J. C.F
– sequence: 3
  fullname: Raymond, C. A
BookMark eNqFkE9vFSEUR4lpE_vHr6As3bwKAwNM4qZp1Jo0dtFWl-Qyc-cVnYEnMGnet5fna5PGhV1xQ875Lc4xOQgxICFvOTvjzLAPjDHZ8dacNYw39UtpJYx4RY4a0bQrxYw-eHa_Jsc5_6yKEpIdkV_fIXkoPgbqA10nxEAHDNmXLYUw0Dn6XJaEtI-hYCg0jjTBUBWgGx-QlqrknVvukV4uM9KE691cBb_hA72JS7mnP2DCfEoOR5gyvnl8T8jd50-3F5erq-svXy_Or1a96GRZOen6pmOibQbltDKKOd2h1k4qwyUK6aQQEsTAB945aMWo2lG2WjKnQDohTsj7_e4mxd8L5mJnn3ucJggYl2y5UkI1otOmomqP9inmnHC0m-RnSFvLmd3VtU917a6ufapbxY__iL0vfzuWBH56WT_f6z6MMc3wENM02ALbKaYxQeh9tuLFjXf7jRGihXWqyt1NRdrKaymN-S-hlGRS_AHUQKcT
CitedBy_id crossref_primary_10_3390_f8110439
crossref_primary_10_1093_forsci_fxae020
crossref_primary_10_1186_s40490_014_0016_5
crossref_primary_10_1186_s40490_015_0048_5
crossref_primary_10_3390_f13030485
crossref_primary_10_1007_s00468_012_0815_3
crossref_primary_10_1016_j_foreco_2017_06_006
crossref_primary_10_1007_s40725_024_00219_3
Cites_doi 10.1038/189678b0
10.1007/1-4020-4393-7_8
10.1104/pp.88.3.574
10.1079/9780851990798.0000
10.1080/00049158.1952.10675282
10.1093/treephys/22.1.21
10.1007/1-4020-4393-7_3
10.1021/ie50347a017
10.1139/x82-086
10.1515/hfsg.1961.15.5.129
10.1111/j.1469-8137.1954.tb05258.x
10.1007/978-3-642-73683-4
10.1111/j.1365-3040.1991.tb00944.x
10.1093/forestry/29.1.5
ContentType Journal Article
Copyright Copyright Taylor & Francis Group, LLC 2012
Copyright_xml – notice: Copyright Taylor & Francis Group, LLC 2012
DBID FBQ
AAYXX
CITATION
7S9
L.6
DOI 10.1080/00049158.2012.10676383
DatabaseName AGRIS
CrossRef
AGRICOLA
AGRICOLA - Academic
DatabaseTitle CrossRef
AGRICOLA
AGRICOLA - Academic
DatabaseTitleList
AGRICOLA


Database_xml – sequence: 1
  dbid: FBQ
  name: AGRIS
  url: http://www.fao.org/agris/Centre.asp?Menu_1ID=DB&Menu_2ID=DB1&Language=EN&Content=http://www.fao.org/agris/search?Language=EN
  sourceTypes: Publisher
DeliveryMethod fulltext_linktorsrc
Discipline Forestry
EISSN 2325-6087
EndPage 42
ExternalDocumentID 10_1080_00049158_2012_10676383
10676383
US201500074488
US201500066404
GeographicLocations New Zealand
New South Wales
GeographicLocations_xml – name: New South Wales
– name: New Zealand
GroupedDBID ..I
0BK
0R~
23N
30N
4.4
5GY
6J9
AAGME
AAHBH
AAJMT
AALDU
AAMIU
AAOAP
AAPUL
AAQRR
ABCCY
ABFIM
ABFMO
ABJNI
ABLIJ
ABPAQ
ABPEM
ABTAA
ABTAH
ABTAI
ABXUL
ABXYU
ACBBU
ACDHJ
ACGFO
ACGFS
ACQMU
ACTIO
ACZPZ
ADCVX
ADGTB
ADGTR
ADOPC
ADYSH
AEISY
AENEX
AEYOC
AFDYB
AFRVT
AGDLA
AHDZW
AI.
AIDBO
AIJEM
AIYEW
AKBVH
AKOOK
ALMA_UNASSIGNED_HOLDINGS
ALQZU
AMATQ
APNXG
AQRUH
AURDB
AVBZW
AWYRJ
BFWEY
BLEHA
C0.
CCCUG
CWRZV
DGEBU
DKSSO
DLOXE
EBS
EJD
E~A
E~B
FBQ
GTTXZ
H13
HGUVV
HZ~
H~P
IPNFZ
JEPSP
KPS
KYCEM
LJTGL
M4Z
NUSFT
O9-
OWHGL
P2P
PCLFJ
RIG
RNANH
ROSJB
RTWRZ
S-T
SJN
SNACF
TBQAZ
TDBHL
TEI
TFL
TFT
TFW
TQWBC
TTHFI
TUROJ
U5U
UT5
VH1
XOL
ZGOLN
ZY4
~02
~KM
AAAVI
ABJVF
ABQHQ
AEGYZ
AFOLD
AFWLO
AHDLD
AIRXU
FUNRP
FVPDL
V1K
AAGDL
AAHIA
AAYXX
AMPGV
CITATION
7S9
L.6
TASJS
ID FETCH-LOGICAL-c394t-b4bc290352d6b76860b79e77b46814e34b4334a3d1d19ba53f65f45740b6a4b33
ISSN 2325-6087
0004-9158
IngestDate Fri Sep 05 17:21:11 EDT 2025
Tue Jul 01 03:53:45 EDT 2025
Thu Apr 24 23:05:40 EDT 2025
Wed Dec 25 09:06:02 EST 2024
Wed Dec 27 19:20:06 EST 2023
Thu Apr 03 09:44:58 EDT 2025
IsPeerReviewed true
IsScholarly true
Issue 1
Language English
LinkModel OpenURL
MergedId FETCHMERGED-LOGICAL-c394t-b4bc290352d6b76860b79e77b46814e34b4334a3d1d19ba53f65f45740b6a4b33
Notes http://dx.doi.org/10.1080/00049158.2012.10676383
ObjectType-Article-1
SourceType-Scholarly Journals-1
ObjectType-Feature-2
content type line 23
PQID 1663623978
PQPubID 24069
PageCount 12
ParticipantIDs proquest_miscellaneous_1663623978
informaworld_taylorfrancis_310_1080_00049158_2012_10676383
fao_agris_US201500066404
crossref_primary_10_1080_00049158_2012_10676383
fao_agris_US201500074488
crossref_citationtrail_10_1080_00049158_2012_10676383
ProviderPackageCode CITATION
AAYXX
PublicationCentury 2000
PublicationDate 2012-00-00
PublicationDateYYYYMMDD 2012-01-01
PublicationDate_xml – year: 2012
  text: 2012-00-00
PublicationDecade 2010
PublicationTitle Australian forestry
PublicationYear 2012
Publisher Taylor & Francis Group
Publisher_xml – name: Taylor & Francis Group
References Ellis J. C. (CIT0014) 2005
Clark J. (CIT0007) 1957; 35
Cown D. J. (CIT0009) 1999
CIT0030
CIT0031
Cown D. J. (CIT0010) 1980; 10
CIT0033
Langrish T. (CIT0023) 2006
Moreno Chan J. (CIT0028) 2010; 64
Harris J. M. (CIT0019) 1961; 189
Loe J. A. (CIT0024) 1953; 7
Cown D. J. (CIT0011) 1982; 12
Alinee B. (CIT0001) 1989
Grace J. (CIT0017) 1993
Wardrop A. B. (CIT0036) 1961; 15
Maclaren J. P. (CIT0025) 2000
Moreno Chan J. (CIT0027) 2007
Cown D. J. (CIT0008) 1974; 4
CIT0015
Uprichard J. M. (CIT0034) 1991
CIT0037
Chalk L. (CIT0005) 1956; 29
Weatherwax R. C. (CIT0038) 1968; 18
Bamber R. K. (CIT0002) 1972; 6
MacLean J. D. (CIT0026) 1952
Harris J. M. (CIT0018) 1954; 53
Stamm A. J. (CIT0032) 1964
Cinnirella S. (CIT0006) 2002; 22
Booker R. E. (CIT0003) 1978; 8
Edwards W. R.N. (CIT0013) 1982; 5
Hughes R. V. (CIT0021) 1949; 3
Kininmonth J. A. (CIT0022) 1991
Wilkes J. (CIT0039) 1991; 25
Harris J. M. (CIT0020) 1991
Cown D. J. (CIT0012) 1991; 50
Walker J. C.F. (CIT0035) 2006
Morris J. (CIT0029) 2005
Fonseca M. A. (CIT0016) 2005
CIT0004
References_xml – volume: 189
  start-page: 678
  year: 1961
  ident: CIT0019
  publication-title: Nature
  doi: 10.1038/189678b0
– start-page: 109
  volume-title: Water Deficits: Plant Responses from Cell to Community.
  year: 1993
  ident: CIT0017
– volume: 4
  start-page: 540
  year: 1974
  ident: CIT0008
  publication-title: New Zealand Journal of Forestry Science
– start-page: 251
  volume-title: Primary Wood Processing: Principles and Practice.
  year: 2006
  ident: CIT0023
  doi: 10.1007/1-4020-4393-7_8
– start-page: 75
  volume-title: New Forests: Wood Production and Environmental Services.
  year: 2005
  ident: CIT0029
– ident: CIT0033
  doi: 10.1104/pp.88.3.574
– volume-title: The Measurement of Roundwood: Methodologies and Conversion Ratios. CABI Publishing, Cambridge MA, 269 pp.
  year: 2005
  ident: CIT0016
  doi: 10.1079/9780851990798.0000
– ident: CIT0015
  doi: 10.1080/00049158.1952.10675282
– volume: 7
  start-page: 183
  year: 1953
  ident: CIT0024
  publication-title: Pinus radiata. APPITA
– volume-title: Preservative Treatment of Wood by Pressure Methods. Agriculture Handbook No. 40. US Department of Agriculture. Washington, DC. 160 pp.
  year: 1952
  ident: CIT0026
– volume: 12
  start-page: 71
  year: 1982
  ident: CIT0011
  publication-title: Pinus radiata. New Zealand Journal of Forestry Science
– volume: 25
  start-page: 85
  year: 1991
  ident: CIT0039
  publication-title: Pinus radiata. Wood Science and Technology
– volume: 8
  start-page: 295
  year: 1978
  ident: CIT0003
  publication-title: New Zealand Journal of Forestry Science
– volume: 3
  start-page: 387
  year: 1949
  ident: CIT0021
  publication-title: APPITA
– volume-title: Wood and Cellulose Science. Ronald Press Co., New York. 549 pp.
  year: 1964
  ident: CIT0032
– volume-title: New Zealand Pine and Douglas Fir: Suitability for Processing. Forest Research Bulletin No. 216. Forest Research Institute, Rotorua, 72 pp.
  year: 1999
  ident: CIT0009
– volume: 22
  start-page: 21
  year: 2002
  ident: CIT0006
  publication-title: Tree Physiology
  doi: 10.1093/treephys/22.1.21
– start-page: 69
  volume-title: Primary Wood Processing: Principles and Practice.
  year: 2006
  ident: CIT0035
  doi: 10.1007/1-4020-4393-7_3
– ident: CIT0031
  doi: 10.1021/ie50347a017
– volume: 10
  start-page: 508
  year: 1980
  ident: CIT0010
  publication-title: New Zealand Journal of Forestry Science
– volume-title: How Much Has Your Woodlot Got? A Practical Guide to Estimating the Volume and Value of Planted Trees. Forest Research Bulletin No. 217. New Zealand Forest Research Institute Ltd, Rotorua.
  year: 2000
  ident: CIT0025
– ident: CIT0037
  doi: 10.1139/x82-086
– start-page: 150
  volume-title: NZIF Forestry Handbook.
  year: 2005
  ident: CIT0014
– volume: 5
  start-page: 271
  year: 1982
  ident: CIT0013
  publication-title: Plant, Cell and Environment
– volume: 6
  start-page: 32
  year: 1972
  ident: CIT0002
  publication-title: P. radiata. Journal of the Institute of Wood Science
– start-page: 4
  volume-title: Properties and Uses of New Zealand Radiata Pine. Volume 1—Wood Properties.
  year: 1991
  ident: CIT0034
– start-page: 379
  volume-title: Cellulose and Wood: Chemistry and Technology.
  year: 1989
  ident: CIT0001
– volume: 15
  start-page: 129
  year: 1961
  ident: CIT0036
  publication-title: Holzforschung
  doi: 10.1515/hfsg.1961.15.5.129
– volume: 18
  start-page: 44
  issue: 7
  year: 1968
  ident: CIT0038
  publication-title: Forest Products Journal
– volume: 50
  year: 1991
  ident: CIT0012
  publication-title: Forest Research Bulletin No.
– volume: 53
  start-page: 517
  year: 1954
  ident: CIT0018
  publication-title: New Phytologist
  doi: 10.1111/j.1469-8137.1954.tb05258.x
– volume: 64
  start-page: 521
  year: 2010
  ident: CIT0028
  publication-title: Holzforschung
– volume: 35
  start-page: 219
  year: 1957
  ident: CIT0007
  publication-title: Further investigation of seasonal changes in moisture content of certain Canadian forest trees. Canadian Journal of Botany
– volume-title: Moisture content in radiata pine wood: implications for wood quality and water-stress response.
  year: 2007
  ident: CIT0027
– start-page: 6
  volume-title: Properties and Uses of New Zealand Radiata Pine. Volume 1—Wood Properties.
  year: 1991
  ident: CIT0020
– ident: CIT0030
  doi: 10.1007/978-3-642-73683-4
– ident: CIT0004
  doi: 10.1111/j.1365-3040.1991.tb00944.x
– volume: 29
  start-page: 6
  year: 1956
  ident: CIT0005
  publication-title: Forestry
  doi: 10.1093/forestry/29.1.5
– start-page: 7
  volume-title: Properties and Uses of New Zealand Radiata Pine. Volume 1—Wood Properties.
  year: 1991
  ident: CIT0022
SSID ssj0046340
Score 1.9204466
Snippet SummaryVariation in green density and moisture content are relevant for log transport planning, weight-scaling systems, lumber drying and dynamic assessment of...
Summary Variation in green density and moisture content are relevant for log transport planning, weight-scaling systems, lumber drying and dynamic assessment...
Variation in green density and moisture content are relevant for log transport planning, weight-scaling systems, lumber drying and dynamic assessment of...
SourceID proquest
crossref
informaworld
fao
SourceType Aggregation Database
Enrichment Source
Index Database
Publisher
StartPage 31
SubjectTerms age structure
climate
drought
drying
heartwood
lumber
moisture content
New South Wales
New Zealand
Pinus radiata
planning
radiata pine
sapwood
trees
Tumut NSW Australia
water content
winter
wood density
wood properties
Title Variation in green density and moisture content of radiata pine trees in the Hume region of New South Wales
URI https://www.tandfonline.com/doi/abs/10.1080/00049158.2012.10676383
https://www.proquest.com/docview/1663623978
Volume 75
hasFullText 1
inHoldings 1
isFullTextHit
isPrint
link http://utb.summon.serialssolutions.com/2.0.0/link/0/eLvHCXMwnV3Nb9MwFLegkxAXxKdWvmQkblVCXDtxzW0qTNUkOEDLJi6RnTjVBEumNTvAX897tpO2tGjAJaqSOony-8nv-z1CXk-UtaBoFFFSqiISWWEjpUoeMazTtKXU2rkGPnzMZgtxcpaerUMxrrqkNXHxc29dyf-gCucAV6yS_Qdk-5vCCfgN-MIREIbjX2H8BQxd3WUrLjGDZlRiQnrrmypdNIAhBggwHz3E_K-wF0GrR5eoXWJEetVlOgKwOEJlGTRITHx08_VGpyBDVptK7KZ_pMHZHutUYixW6MquMQwEl-tmw2kfcjhO4tE07nOKP-kfF2G68TQOztXgiGBrg3W-Mw1kw3HmtjJQ29IoS4JoDfuun5iyxS-_iQax4MWx7721s9H3mZFCsdSl6I1j7IYH2wlfi7Y-4XDxeYyuHVSwBHaPPRhLydIBOTiavft62olukXFXQdu_bldSjs3Y9z5qS5u5Xenmt463OxLeqS3z--ResDfokSfPA3LL1g_JneMA2yPyrecQPa-p4xANHKLAIdpxiAYO0aaigUMUOUQdh3AtcIgih6jnEP4ROEQdh6jj0GOyOH4_n86iMIAjKrgSbWSEKcYKO-aWmQG7NEuMVFZKI7IJE5YLIzgXmpesZMrolFdZWolUisRkWhjOn5BB3dT2kNBxwZgFa7kqRCFKbiYTJstKMVXKRILUGZK0-5B5EbrT45CU7znrm9h6AHIEIO8AGJI3_bpL35_lxhWHgFOulyBE821e7L8kBQi5IXm7iWveOs5Xnu45v-mRrzoW5LB7Y0hO17a5XuUMFH4wQJScPP3zaz0jd_F23vH3nAzaq2v7AlTh1rwMBP4FkqenwQ
linkProvider Library Specific Holdings
linkToHtml http://utb.summon.serialssolutions.com/2.0.0/link/0/eLvHCXMwpV1Lb9QwELbaIgGXlqe6PI3ENdt4PYljbqhqtUC7F7rQm-VXKlRIqt3sAX59Z5xNBQXUQ8-O7dgej78Zj79h7G2lY0Sg4bM8aJ9B6WOmdZCZoHeaMShrk2vgeFZO5_DxtDjdYPvDWxgKqyQbuu6JIpKups1NzughJG4v4VpRpMisyZhI0FCK5Ca7UyB4JzGX-WxQx1BK6N-h5JBRpeGZ8H_b-eOE2qxte43F9C-tnY6iwx0WhkH0ESjn41Xnxv7XNX7HW47yAdteQ1X-vpeth2wjNo_YXcrlSQniHrPzL2hnp4Xl3xp-RgE8PFA8fPeTY6_8R4sitFpETuHweLbxtuYLokLoLL_A_-F0Ib6kughCOcpV5JQmApvDD1H58pTej3_FI2z5hM0PD072p9k6d0PmpYYuc-D8RBPZaigdmjRl7pSOSjkoKwFRggMpwcoggtDOFrIuixoKBbkrLTgpn7Ktpm3iLuMTL0REQ6v24CFIV1VChVoLHVSuUGGNWDGsl_FrYnPKr_HdiCv-034mDc2kGWZyxPau6l301B431thFcTD2DPWvmX-ekLeIMBvk8O8ihcZvNWLvfhcf0yVXTN3nTTHypi7fDMJmcOPTbY5tYrtaGoFYEbGrVtWz23Twmt2bnhwfmaMPs0_P2X0q6z1ML9hWt1jFl4i5Ovcq7alLdG4WHQ
linkToPdf http://utb.summon.serialssolutions.com/2.0.0/link/0/eLvHCXMwpV1Lb9QwELZokSouUF7qAgUjcc02Xk_smBuiXZXXCgkWerPiRypUSFa72QP8emacTVUKqIeeHduxPR5_Mx5_w9iL0sSIQMNneTA-A-VjZkyQmaB3mjHoqkqugQ8zdTyHtyfFyYW3MBRWSTZ03RNFJF1Nm3sR6iEi7iDBWlGkwKzJmDjQUIjkFrupEJ9QWJ_MZ4M2BiWhf4aSQ0aVhlfC_23njwNqq67aSySmfyntdBJN7zA_jKEPQDkbrzs39r8u0Tteb5C77PYGqPJXvWTdZTdic4_tUCZPSg93n519QSs7LSv_1vBTCt_hgaLhu58cO-U_WhSg9TJyCobHk423NV8SEUJX8QX-Dqfr8BXVRQjKUaoipyQR2Bx-iKqXp-R-_CseYKsHbD49-vz6ONtkbsi8NNBlDpyfGKJaDcqhQaNyp03U2oEqBUQJDqSESgYRhHFVIWtV1FBoyJ2qwEn5kG03bRP3GJ94ISKaWbUHD0G6shQ61EaYoHON6mrEimG5rN_QmlN2je9WnLOf9jNpaSbtMJMjdnBeb9ETe1xZYw-lwVanqH3t_NOEfEWE2CCHfxdpNH3LEXt5UXpslxwxdZ81xcqrunw-yJrFbU93OVUT2_XKCkSKiFyNLh9dp4NnbOfj4dS-fzN795jdoqLevfSEbXfLddxHwNW5p2lH_QbXtBTB
openUrl ctx_ver=Z39.88-2004&ctx_enc=info%3Aofi%2Fenc%3AUTF-8&rfr_id=info%3Asid%2Fsummon.serialssolutions.com&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Ajournal&rft.genre=article&rft.atitle=Variation+in+green+density+and+moisture+content+of+radiata+pine+trees+in+the+Hume+region+of+New+South+Wales&rft.jtitle=Australian+forestry&rft.au=Chan%2C+Julian+Moreno&rft.au=Walker%2C+J.+C.F&rft.au=Raymond%2C+C.+A&rft.date=2012&rft.pub=Taylor+%26+Francis+Group&rft.issn=2325-6087&rft.volume=75&rft.issue=1&rft.spage=31&rft.epage=42&rft_id=info:doi/10.1080%2F00049158.2012.10676383&rft.externalDocID=US201500066404
thumbnail_l http://covers-cdn.summon.serialssolutions.com/index.aspx?isbn=/lc.gif&issn=2325-6087&client=summon
thumbnail_m http://covers-cdn.summon.serialssolutions.com/index.aspx?isbn=/mc.gif&issn=2325-6087&client=summon
thumbnail_s http://covers-cdn.summon.serialssolutions.com/index.aspx?isbn=/sc.gif&issn=2325-6087&client=summon