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创新是引领学科发展的动力源泉。在中科院、国家科技部、国家自然科学基金委和广东省的长期支持下,中科院华南植物园鼎湖山森林生态系统定位研究站(以下简称"鼎湖山站")以长期监测与创新研究为手段,发现成熟森林土壤持续积累有机碳现象,从宏观到微观的不同尺度阐明森林土壤积累有机碳的机理及其驱动机制,引领森林生态系统碳氮水循环过程及其耦合对环境变化的响应与适应规律的研究,推动生态系统非平衡理论的建立;科学量化了全国森林生态系统碳汇现状与潜力,为国家环境外交提供了重要的科学支撑;提出森林与产水量的全球模式并精确给出了控制产水量气候与流域特征参数的临界值,为"森林与产水量"关系的争论提供了新的阐释;发现常绿阔叶林群落适应气候变化在过去30年向灌丛化方向演替并阐明其受主要环境因子影响的机理。研究成果为森林固碳与水资源效应的科学评估、自然保护区和生态环境建设的国家需求提供了理论支撑。鼎湖山站成为国内外无可替代的野外科技支撑平台和国际著名的森林生态系统科学研究基地,也是中科院和广东地区生态学人才培养基地。 相似文献
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Sap flow and environmental conditions were monitored at two Eucalyptus (Eucalyptus urophylla S.T.Blake)plantations at Hetou and Jijia, located in Leizhou, Zhanjiang, Guangdong Province. It was found that daily sap flux density (SFD) of Eucalyptus was closely related to daily atmospheric vapor pressure deficit (VPD) (R2=0.76, P=0.01 at Hetou and R2=0.7021, P=0.01 at Jijia) at both sites. No significant relationship existed between daily SFD and mean daily air temperature at both sites. Daily SFD varied with wind speed Y=-17585X3 15147X2-1250.7X 2278.4 (R2=0.68; P=0.01) at Hetou and Y=-101.67X3-1.65X2-376.4X 1914.8 (R2=0.40, P=0.05) at Jijia, where Ywas daily SFD, Xwas daily wind speed.Experimental observations yielded the following data: (1) the critical lower and upper daily VPD threshold were 0 and 2 kPa,slightly lower under high relative humidity (＞80%) compared with those at the Jijia site; (3) The upper and lower threshold 相似文献
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Sap flow and environmental conditions were monitored at two Eucalyptus (Eucalyptus urophylla S.T.Blake) plantations at Hetou and Jijia, located in Leizhou, Zhanjiang, Guangdong Province. It was found that daily sap flux density (SFD) of Eucalyptus was closely related to daily atmospheric vapor pressure deficit (VPD) (R2=0.76, P=0.01 at Hetou and R2=0.7021, P=0.01 at Jijia) at both sites. No significant relationship existed between daily SFD and mean daily air temperature at both sites. Daily SFD varied with wind speed Y=-17585X3 15147X2-1250.7X 2278.4 (R2=0.68; P=0.01) at Hetou and Y=-101.67X3-1.65X2-376.4X 1914.8 (R2=0.40,P=0.05) at Jijia, where Y was daily SFD,X was daily wind speed. Experimental observations yielded the following data: (1) the critical lower and upper daily VPD threshold were 0 and 2 kPa, within which daily SFD varied from 540±70 L/(m2·d) to 4739±115 L/(m2·d) at Hetou site, from 397±26 L/(m2·d) to 3414±191 L/(m2·d) at Jijia site; (2) Diurnal SFDs at Hetou site were much highe 相似文献
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