Published Date
, Volume 20, Issue 1, pp 85–93
Original Article
Cite this article as:
Moon, M., Kim, T., Park, J. et al. J For Res (2015) 20: 85. doi:10.1007/s10310-014-0463-0
Abstract
Accurate estimates of stand transpiration (E) require the consideration of three types of variation in sap flux density (JS): radial, azimuthal, and tree-to-tree variation. In this study, the JS variation of 50-year-old Korean pine (Pinus koraiensis) trees and its effect on Eestimates was evaluated using Granier-type heat dissipation sensors. The value of JSdecreased exponentially with the radial depth from cambium to pith, and the coefficient of variation (CV) for radial variation was 124.3 %. Regarding the azimuthal variation, the value of JS differed significantly among aspects and the average CV was 23.6 %. The average CV for tree-to-tree variation was 34.0 %, and the daily CV increased with increasing vapor pressure deficit (D). The error in the E estimates caused by ignoring the radial variation was the largest (109.2 %), followed by those caused by ignoring the tree-to-tree and azimuthal variations (24.3 and 12.6 %, respectively). While the contribution of the azimuthal variation to the E estimates was minimal in comparison to the other variations, the azimuthal variation among aspects was significant, and the usage of the north aspect measurement did not generate substantial error in the E estimates (0.6 %). Our results suggest that the variation, particularly the species- and site-specific radial variation, must be considered when accurately calculating E estimates.
References
For further details log on website :
http://link.springer.com/article/10.1007/s10310-014-0463-0
, Volume 20, Issue 1, pp 85–93
Original Article
- First Online:
- 12 September 2014
DOI: 10.1007/s10310-014-0463-0
Title
Variation in sap flux density and its effect on stand transpiration estimates of Korean pine stands
Abstract
Accurate estimates of stand transpiration (E) require the consideration of three types of variation in sap flux density (JS): radial, azimuthal, and tree-to-tree variation. In this study, the JS variation of 50-year-old Korean pine (Pinus koraiensis) trees and its effect on Eestimates was evaluated using Granier-type heat dissipation sensors. The value of JSdecreased exponentially with the radial depth from cambium to pith, and the coefficient of variation (CV) for radial variation was 124.3 %. Regarding the azimuthal variation, the value of JS differed significantly among aspects and the average CV was 23.6 %. The average CV for tree-to-tree variation was 34.0 %, and the daily CV increased with increasing vapor pressure deficit (D). The error in the E estimates caused by ignoring the radial variation was the largest (109.2 %), followed by those caused by ignoring the tree-to-tree and azimuthal variations (24.3 and 12.6 %, respectively). While the contribution of the azimuthal variation to the E estimates was minimal in comparison to the other variations, the azimuthal variation among aspects was significant, and the usage of the north aspect measurement did not generate substantial error in the E estimates (0.6 %). Our results suggest that the variation, particularly the species- and site-specific radial variation, must be considered when accurately calculating E estimates.
References
- Alvarado-Barrientos MS, Hernández-Santana V, Asbjornsen H (2013) Variability of the radial profile of sap velocity in Pinus patula from contrasting stands within the seasonal cloud forest zone of Veracruz, Mexico. Agric For Meteorol 168:108–119CrossRef
- Barij N, Čermák J, Stokes A (2011) Azimuthal variations in xylem structure and water relations in cork oak (Quercus suber). Iawa J 32:25–40CrossRef
- Caylor KK, Dragoni D (2009) Decoupling structural and environmental determinants of sap velocity. Part I. Methodological development. Agric For Meteorol 149:559–569
- Cermak J, Nadezhdina N (1998) Sapwood as the scaling parameter defining according to xylem water content or radial pattern of sap flow? Ann For Sci 55:509–521CrossRef
- Čermák J, Kučera J, Nadezhdina N (2004) Sap flow measurements with some thermodynamic methods, flow integration within trees and scaling up from sample trees to entire forest stands. Trees Struct Funct 18:529–546CrossRef
- Chang X, Zhao W, He Z (2014) Radial pattern of sap flow and response to microclimate and soil moisture in Qinghai spruce (Picea crassifolia) in the upper Heihe river basin of arid northwestern China. Agric For Meteorol 187:14–21
- Dye PJ, Olbrich BW, Poulter AG (1991) The influence of growth rings in Pinus patula on heat pulse velocity and sap flow measurement. J Exp Bot 42:867–870CrossRef
- Ford CR, Hubbard RM, Kloeppel BD, Vose JM (2007) A comparison of sap flux-based evapotranspiration estimates with catchment-scale water balance. Agric For Meteorol 145:176–185CrossRef
- Granier A (1985) Une nouvelle méthode pour la mesure du flux de sève brute dans le tronc des arbres. Ann For Sci 42:193–200CrossRef
- Granier A, Biron P, Breda N, Pontailler JY, Saugier B (1996) Transpiration of trees and forest stands: short and long-term monitoring using sapflow methods. Glob Chang Biol 2:265–274CrossRef
- Jimenez E, Vega JA, Perez-Gorostiaga P, Fonturbel T, Fernandez C (2010) Evaluation of sap flow density of Acacia melanoxylon R. Br. (blackwood) trees in overstocked stands in north-western Iberian Peninsula. Eur J Forest Res 129:61–72CrossRef
- Köstner B, Granier A, Cermák J (1998) Sapflow measurements in forest stands: methods and uncertainties. Ann For Sci 55:13–27CrossRef
- Kumagai T, Aoki S, Nagasawa H, Mabuchi T, Kubota K, Inoue S, Utsumi Y, Otsuki K (2005) Effects of tree-to-tree and radial variations on sap flow estimates of transpiration in Japanese cedar. Agric For Meteorol 135:110–116CrossRef
- Kume T, Onozawa Y, Komatsu H, Tsuruta K, Shinohara Y, Umebayashi T, Otsuki K (2010a) Stand-scale transpiration estimates in a Moso bamboo forest. (I) Applicability of sap flux measurements. For Ecol Manage 260:1287–1294
- Kume T, Otsuki K, Du S, Yamanaka N, Wang YL, Liu GB (2012) Spatial variation in sap flow velocity in semiarid region trees: its impact on stand-scale transpiration estimates. Hydrol Process 26:1161–1168CrossRef
- Lagergren F, Lindroth A (2004) Variation in sapflow and stem growth in relation to tree size, competition and thinning in a mixed forest of pine and spruce in Sweden. For Ecol Manage 188:51–63CrossRef
- Oren R, Phillips N, Katul G, Ewers BE, Pataki DE (1998) Scaling xylem sap flux and soil water balance and calculating variance: a method for partitioning water flux in forests. Ann For Sci 55:191–216CrossRef
- Phillips N, Oren R, Zimmermann R (1996) Radial patterns of xylem sap flow in non-, diffuse-and ring-porous tree species. Plant Cell Environ 19:983–990CrossRef
- Ryu D, Moon M, Park J, Cho S, Kim T, Kim HS (2014) Development of allometric equations for V age-class Pinus koraiensis in Mt. Taehwa plantation Gyeonggi-do. Kor J Agric For Meteorol 16:29–38CrossRef
- Tateishi M, Kumagai T, Utsumi Y, Umebayasi T, Shiiba Y, Inoue K, Kaji K, Cho K, Otsuki K (2008) Spatial variations in xylem sap flux density in evergreen oak trees with radial-porous wood: comparisons with anatomical observations. Trees Struct Funct 22:23–30
- Tsuruta K, Kume T, Komatsu H, Higashi N, Umebayashi T, Kumagai T, Otsuki K (2010) Azimuthal variations of sap flux density within Japanese cypress xylem trunks and their effects on tree transpiration estimates. J For Res 15:398–403CrossRef
- Wilson KB, Hanson PJ, Mulholland PJ, Baldocchi DD, Wullschleger SD (2001) A comparison of methods for determining forest evapotranspiration and its components: sap-flow, soil water budget, eddy covariance and catchment water balance. Agric For Meteorol 106:153–168CrossRef
For further details log on website :
http://link.springer.com/article/10.1007/s10310-014-0463-0
No comments:
Post a Comment