首页> 外文会议>Conference on Remote Sensing for Agriculture, Ecosystems, and Hydrology II 25-27 September 2000 Barcelona, Spain >Water budget model of Eucalyptus FOrest using a canopy characterization by Remote Sensing techniques and a soil water flux parameterization
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Water budget model of Eucalyptus FOrest using a canopy characterization by Remote Sensing techniques and a soil water flux parameterization

机译:桉树冠层水分收支模型的遥感冠层表征和土壤水分通量参数化。

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This paper deals with the development of a water budget model for Eucalyptus forest, using a conceptually simple one-dimensional mass balance approach within the root zone of the forest. The model uses Leaf ARea Index to quantify the forest structure important for mass and energy exchange, and this represents a key simplification for regional scale applications. Remote Sensing vegetation indexes and mixture modeling techniques were used to estimate LAI. A five-layered water balance model, with water movement between layers along hydraulic gradients, was develoepd and parameterized for a eucalypt plantation (Eucalyptus grandis Hill ex. Maiden hybrids) in Brazil. Available soil water controls stomatal conductance and hence transpiration, which is calculated by the Penman-Monteith equation. The remote sensing derived LAI was used to compute the canopy conductance that drives the Penman-Monteith formulation. The model accounts for changes in the depths of the water table. The test period was from October 1995 to September 1996 in a nine-year-old plantation in an experimental catchment in eastern Brazil. Total transpiration for the year was 1116 mm, with 119 mm intercepted and re-evaporated and another 79 mm soil surface evaporation, giving evapotranspiration of 1314 mm compared to rainfall of 1396 mm. The water balance was closed by not flow below the root zone of about 53 mm and an increase in water storage (in the first layer) of 29 mm. The model also estimated a water deficit of 135 mm (difference between the potential and current transpiration) for the period. Upward flux from the water table was around 81 mm and piezometric measurements showed 1.5 m recession for the same period. The upward flux into the root zone was about 1 mm day~(-1) at the end of a long dry season; that kept the water storage in that zone to about 15percent of capacity and helped prevent complete stomatal closure. Comparison between esimated water storage and measurements confirmed that this model is a very promising tool for calculating water use by plantations. It can also provide water balance information and information about stomatal conductance for growth prediction models.
机译:本文使用在森林根部区域内的概念上简单的一维质量平衡方法,来处理桉树森林的水预算模型。该模型使用Leaf ARea Index来量化对于质量和能量交换很重要的森林结构,这代表了区域规模应用的关键简化。利用遥感植被指数和混合模型技术估算了LAI。开发了一个五层水平衡模型,其中各层之间沿着水力梯度进行水运动,并为巴西的桉树人工林(Eucalyptus grandis Hill ex。Maiden hybrids)参数化。可用的土壤水控制气孔导度,从而控制蒸腾作用,这是通过Penman-Monteith方程计算的。遥感得出的LAI用于计算驱动Penman-Monteith公式的冠层电导。该模型考虑了地下水位深度的变化。试验期为1995年10月至1996年9月,在巴西东部一个实验流域的一个有9年历史的人工林中。全年总蒸发量为1116毫米,其中119毫米被截留并再次蒸发,另外79毫米土壤表面蒸发,蒸发蒸腾量为1314毫米,而降雨量为1396毫米。通过在约53mm的根部区域以下不流动并关闭29mm的储水量(第一层)来关闭水平衡。该模型还估计该时期的缺水量为135毫米(势能和当前蒸腾量之间的差异)。地下水位的向上通量约为81 mm,测压测量结果显示同一时期内有1.5 m的后退。在较长的旱季结束时,流入根区的通量约为1毫米天(-1)。使该区域的蓄水量保持在容量的15%左右,并有助于防止气孔完全闭合。模拟蓄水量和测量值之间的比较证实,该模型是用于计算人工林用水量的非常有前途的工具。它还可以为生长预测模型提供水平衡信息和有关气孔导度的信息。

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