刺槐蒸腾耗水的动态研究(英文)

The Dynamic Study on Transpiration Consumption of Black Locust Forest

推算林分的年总耗水量 ,首先要确定林分的年总蒸腾量 .该文以LI 16 0 0稳态气孔仪在 1998～2 0 0 0年生长季各月典型天气的实测数据和常规气象数据为基础 ,应用Penman Monteith方程模拟了刺槐林的日蒸腾过程 ,并以此计算了生长季的连续日蒸腾 .刺槐林林冠层截留净辐射由实测数据 (Rn)与叶面积指数 (LAI)建立的消光系数 (k)数学关系确定 ,冠层整体气孔阻力由实测数据拟合经验式计算 .经与实测结果对比 ,模拟的相对误差平均在 12 %以内 .由全年连续日蒸腾模拟计算 ,1998年至2 0 0 0年 5月～ 10月生长季不同密度刺槐林的平均总蒸腾量分别为 192 4 6 ,187 0 7和 195 5 9mm .

To know the annual water consumption of forest, it is necessary to acquire the annual transpiration value of stands. This paper is based on the data measured in the typical weather of the growth season, from 1998 to 2000, with the LI 1600 Steady Porometer and the general weather information. The daily variation of transpiration in black locust forest ( Robinia pesudoacacia L.) is modeled by Penman Monteith equation. As a result of the model, a continuous daily transpiration in the growth season was calculated. The net radiation, intercepted by black locust forest canopy, was acquired from a semi empirical equation of measuring net radiation R n with the extinction coefficient k and leaf area index LAI . The canopy integral stomatic resistance is a mimesis with an empirical equation of measuring data. Compared with measuring data, the relative error of the modeled ones is less than 12% averagely. At last, the total transpiration of black locust forest during the period of 1998 and 2000 in the growth season of May to October, as an average transpiration of the different density stands, were 192 46, 187 07 and 195 59?mm respectively.