首页> 外文期刊>Annals of Forest Research >Effects of soil water decline on diurnal and seasonal variations in sap flux density for differently aged Japanese cypress (Chamaecyparis obtusa) trees
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Effects of soil water decline on diurnal and seasonal variations in sap flux density for differently aged Japanese cypress (Chamaecyparis obtusa) trees

机译:土壤水分减少对不同年龄的日本柏树(Chamaecyparis obtusa)树液流密度日变化和季节性的影响

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The effects of soil drought on transpiration are often neglected?when predicting transpiration for forests in humid regions under the influence?of the Asian monsoon. These effects have indeed been neglected?for Japanese cypress, Chamaecyparis obtusa, a major plantation species in?Japan and the surrounding area, probably because previous studies have?reported no clear effects of soil drought on transpiration for Japanese cypress?forests. However, a few studies have reported an apparent reduction?in transpiration with soil drought for young Japanese cypress forests. It remains?unclear whether such a reduction in transpiration is limited to young?Japanese cypress forests or if it is not uncommon for mature Japanese cypress?forests, which occupy a large area in Japan. To clarify this point,?we conducted sap flux measurements in a year with soil drought on three?differently aged Japanese cypress stands including mature (43 years old)?and relatively young (23 and 26 years old) trees. In a diurnal time scale, a?cross correlation analysis of sap flux density (Fd) and vapor pressure deficit?(VPD) showed that the time lags between Fd and VPD were 1-3 h in dry?soil conditions. These were larger than those of wet soil conditions (<1 h)?for all sample trees. Fd at a given VPD in dry soil conditions was smaller?than that in wet soil conditions for all sample trees; a 28%–63% reduction?in the rate of change in Fd was observed under dry soil conditions. Because?our results were obtained when the non-exceedance probability of recorded?monthly precipitation was 9%–18%, the results suggest the need to consider?the effects of soil drought more extensively. Those effects should be?considered for not only relatively young but also mature Japanese cypress?when predicting diurnal and seasonal patterns of transpiration in years with?soil drought, and when predicting inter-annual patterns of transpiration for?Japanese cypress despite humid temperate climate.
机译:在预测亚洲季风影响下潮湿地区森林的蒸腾作用时,往往忽略了土壤干旱对蒸腾作用的影响。对于日本柏和日本及周边地区的主要种植树种,日本柏确实被忽略了这些影响,这可能是因为先前的研究没有报告土壤干旱对日本柏林蒸腾作用的明显影响。但是,一些研究报告说,日本年轻的柏树森林的土壤干旱使蒸腾作用明显降低。目前尚不清楚这种蒸腾作用的减少是否仅限于年轻的日本柏树林,还是在日本占很大面积的成熟的日本柏树林并不罕见。为了阐明这一点,我们在一年中土壤干旱的情况下,对三棵不同年龄的日本柏树(包括成熟(43岁)和相对年轻(23岁和26岁)的树木)进行了树液通量测量。在昼夜尺度上,对树液通量密度(Fd)和蒸气压亏缺量(VPD)的相关分析表明,在干燥土壤条件下,Fd和VPD之间的时滞为1-3小时。对于所有样本树来说,这些值都大于潮湿土壤条件(<1 h)?对于所有样本树,在给定的VPD下,干土壤条件下的Fd均小于湿土壤条件下的Fd。在干燥的土壤条件下,Fd的变化率降低了28%-63%。因为我们的结果是在记录的每月降水超额概率为9%–18%时获得的,所以该结果表明需要更广泛地考虑土壤干旱的影响。当预测土壤干旱年份的蒸腾日变化和季节性变化时,以及预测尽管气候温和的日本柏的年蒸发模式时,不仅要考虑相对年轻的日本柏,还要考虑成熟的日本柏。

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