江西千烟洲湿地松人工林碳蓄积及其与水分的关系
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国家重点基础研究发展规划资助项目(2002CB4125);国家科技部国际合作资助项目(2006DFB91920);中国科学院野外台站基金资助项目


Carbon sequestration of Pinus elliottii plantation in relation with water consumption in subtropical China
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    摘要:

    为揭示人工造林对碳循环的贡献以及碳蓄积同水分利用的关系,通过树干解析方法建立南方湿地松(Pinus elliottii)生长模型,并利用树干液流计测定水分消耗过程,分析了从个体到群落尺度的生物量积累特征以及水分消耗规律,包括材积方程、生物量方程、树木生长方程,同时计算单位面积年耗水量及其与生物量积累的相关关系。试验区内湿地松的直径连年生长量从造林初期开始就一直呈下降趋势; 20年生的湿地松人工林密度为1 599株/hm2 (初植密度5000株/hm2),蓄积量为157 m3/hm2,最大蓄积量为209 m3/hm2。目前湿地松林地上生物量为72.061 t/hm2,生物量积累速率为8 493 kg/(hm2·a)(折合碳约为4 370 kg/(hm2·a)),与通量观测得到的净交换量(NEE)结果基本一致。树干液流测定结果显示,湿地松树干液流速度平均为21 495 cm3/(cm2·a),林地通过树木蒸腾耗散的水分为4 769.643 t/(hm2·a),相当于477 mm的降水量,为全年降水的48%;最大耗水量相当于634 mm降水;水分消耗量与地上干物质形成的比例为562∶1,将生物生长量折算成蓄积量计算则水分消耗系数为1091∶1。NPP与林分耗水速度之间呈显著的正相关关系,包括日变化和月变化。

    Abstract:

    Based on stem analysis and sap flow measurement, this study was conducted in subtropical China to clarify the primary productivity and the contribution of afforestation to carbon cycling, as well as the coupling relationship between carbon sequestration and water use. The growth model for Pinus elliottii was established, including volume table, biomass equation, diameter increment etc. Sap flow was measured for interpreting the relationship of primary productivity with water use. The diameter increment declined even from the beginning of afforestation, which implies the inadaptability of the exotic species in China. The stand density was reduced from the initial 5 000 stems/hm2 to the present 1 599 stems/hm2 in 20 years by self thinning. The stand stock was 157 m3/hm2 with its maximum of 209 m3/hm2, and the volume increment was 22 m3/(hm2 a). The above-ground biomass was 72.061 t/hm2, and its growth rate was 8 493 kg/(hm2 a) or 4 370 kgC/(hm2 a), which is approximately consistent with the result (NEE) by means of eddy covariance. The sap flow velocity was 21 495 cm3/(cm2 a), and the total transpiration through canopy layer was 4 769.643 t/(hm2 a) or 477 mm in terms of precipitation, which accounted for 48% of the annual rainfall. The maximum sap flow per year was about 634 mm. The ratio between water consumption and dry matter accumulation was 562∶1. There was a significantly positive correlation between NPP and sap flow velocity, in both daily value and monthly average.

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刘琪璟,曾慧卿,马泽清.江西千烟洲湿地松人工林碳蓄积及其与水分的关系.生态学报,2008,28(11):5322~5330

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