植物学报
植物學報
식물학보
ACTA BOTANICA SINICA
2004年
2期
202-210
,共9页
周国逸%尹光彩%Jim MORRIS%白嘉雨%陈少雄%褚国伟%张宁南
週國逸%尹光綵%Jim MORRIS%白嘉雨%陳少雄%褚國偉%張寧南
주국일%윤광채%Jim MORRIS%백가우%진소웅%저국위%장저남
桉树人工林%水分消耗%树液流通量密度(SFD)%空气饱和差(VPD)%蒸腾作用%蒸散作用
桉樹人工林%水分消耗%樹液流通量密度(SFD)%空氣飽和差(VPD)%蒸騰作用%蒸散作用
안수인공림%수분소모%수액류통량밀도(SFD)%공기포화차(VPD)%증등작용%증산작용
Eucalyptus urophyllaplantation%water consumption%sap flux density (SFD)%vapor pressure deficit (VPD)%transpiration%evapotranspiration
通过对广东省湛江市雷州半岛桉树(Eucalyptus urophylla S.T.Blake)人工林的树液流通量、环境因子、土壤蒸发、林冠截留和林分特性相关指标一年多的连续观测,以及通过一个理论公式对日蒸散量的计算,得出了如下结论:(1)土壤特性及由此决定的土壤水势对树液流通量,以及树液流通量密度(SFD)与气温的关系有一定影响;(2)林冠层的VPD(空气饱和差)对SFD有显著影响;(3)由测定和计算得来的蒸散量在河头和纪家分别有5.26%和6.14%的偏差,可以认为这两种方法有较好的一致性;(4)河头和纪家的林分蒸腾量占总蒸散量百分比分别为62.2%和51.3%;(5)树种单位叶面积水平上的SFD是评价该树种水分利用的重要指标.
通過對廣東省湛江市雷州半島桉樹(Eucalyptus urophylla S.T.Blake)人工林的樹液流通量、環境因子、土壤蒸髮、林冠截留和林分特性相關指標一年多的連續觀測,以及通過一箇理論公式對日蒸散量的計算,得齣瞭如下結論:(1)土壤特性及由此決定的土壤水勢對樹液流通量,以及樹液流通量密度(SFD)與氣溫的關繫有一定影響;(2)林冠層的VPD(空氣飽和差)對SFD有顯著影響;(3)由測定和計算得來的蒸散量在河頭和紀傢分彆有5.26%和6.14%的偏差,可以認為這兩種方法有較好的一緻性;(4)河頭和紀傢的林分蒸騰量佔總蒸散量百分比分彆為62.2%和51.3%;(5)樹種單位葉麵積水平上的SFD是評價該樹種水分利用的重要指標.
통과대광동성담강시뇌주반도안수(Eucalyptus urophylla S.T.Blake)인공림적수액류통량、배경인자、토양증발、림관절류화림분특성상관지표일년다적련속관측,이급통과일개이론공식대일증산량적계산,득출료여하결론:(1)토양특성급유차결정적토양수세대수액류통량,이급수액류통량밀도(SFD)여기온적관계유일정영향;(2)림관층적VPD(공기포화차)대SFD유현저영향;(3)유측정화계산득래적증산량재하두화기가분별유5.26%화6.14%적편차,가이인위저량충방법유교호적일치성;(4)하두화기가적림분증등량점총증산량백분비분별위62.2%화51.3%;(5)수충단위협면적수평상적SFD시평개해수충수분이용적중요지표.
During the period of September 12, 1999 to September 24, 2000, we measured sap flow of eucalyptus (Eucalyptus urophylla S.T. Blake) plantations using heat pulse technique, and the relevant environmental vaiables, such as soil evaporation and canopy interception, etc, at Hetou and Jijia sites,Leizhou Peninsula, Guangdong Province. Based on the measurements of sap flow and estimates of evapotranspiration, the following can be concluded: (1) the maximum of diurnal xylem sap flux density (SFD) at Hetou, where covered with coarse-textured soils formed on Quaternary sediments, was almost twice of that at Jijia, where located on clay-rich soils derived from basalt; (2) SFD was highly correlated to water vapor pressure deficit (VPD) of ambient air near the canopy layer; (3) the correlation between SFD and air temperature also depends on soil properties and soil water potential; (4) the relative differences between measured and modeled evapotranspiration were small, being 5.26% at Hetou and 6.14% at Jijia; (5) the plantation transpiration accounted for 62.2% and 51.3% of the evapotranspiration at Hetou and Jijia,respectively; and (6) the averaged SFD per unit leaf area (ASPULA) was a good index to estimate the amount of water consumption of tree species.