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巴西塞拉多生态系统中树种间土壤水分的分配

Partitioning of soil water among tree species in a Brazilian Cerrado ecosystem.

作者信息

Jackson Paula C., Meinzer Frederick C., Bustamante Mercedes, Goldstein Guillermo, Franco Augusto, Rundel Philip W., Caldas Linda, Igler Erica, Causin Fabio

机构信息

Department of Biology, University of California, Los Angeles, CA 90024, USA.

出版信息

Tree Physiol. 1999 Sep;19(11):717-724. doi: 10.1093/treephys/19.11.717.

Abstract

Source water used by woody perennials in a Brazilian savanna (Cerrado) was determined by comparing the stable hydrogen isotope composition (deltaD) of xylem sap and soil water at different depths during two consecutive dry seasons (1995 and 1996). Plant water status and rates of water use were also determined and compared with xylem water deltaD values. Overall, soil water deltaD decreased with increasing depth in the soil profile. Mean deltaD values were -35 per thousand for the upper 170 cm of soil and -55 per thousand between 230 and 400 cm depth at the end of the 1995 dry season. Soil water content increased with depth, from 18% near the surface to about 28% at 400 cm. A similar pattern of decreasing soil water deltaD with increasing depth was observed at the end of the 1996 dry season. Patterns consistent with hydraulic lift were observed in soil profiles sampled in 1995 and 1997. Concurrent analyses of xylem and soil water deltaD values indicated a distinct partitioning of water resources among 10 representative woody species (five deciduous and five evergreen). Among these species, four evergreen and one deciduous species acquired water primarily in the upper soil layers (above 200 cm), whereas three deciduous and one evergreen species tapped deep sources of soil water (below 200 cm). One deciduous species exhibited intermediate behavior. Total daily sap flow was negatively correlated with xylem sap deltaD values indicating that species with higher rates of water use during the dry season tended to rely on deeper soil water sources. Among evergreen species, minimum leaf water potentials were also negatively correlated with xylem water deltaD values, suggesting that access to more readily available water at greater depth permitted maintenance of a more favorable plant water status. No significant relationship between xylem water deltaD and plant size was observed in two evergreen species, suggesting a strong selective pressure for small plants to rapidly develop a deep root system. The degree of variation in soil water partitioning, leaf phenology and leaf longevity was consistent with the high diversity of woody species in the Cerrado.

摘要

通过比较两个连续旱季(1995年和1996年)不同深度的木质部汁液和土壤水的稳定氢同位素组成(δD),确定了巴西热带稀树草原(塞拉多)木本多年生植物所使用的源水。还测定了植物的水分状况和用水速率,并与木质部水δD值进行比较。总体而言,土壤水δD值随土壤剖面深度增加而降低。在1995年旱季结束时,土壤上层170厘米处的平均δD值为-35‰,在230至400厘米深度之间为-55‰。土壤含水量随深度增加,从地表附近的18%增加到400厘米处的约28%。在1996年旱季结束时,也观察到土壤水δD值随深度增加而降低的类似模式。在1995年和1997年采集的土壤剖面中观察到了与水力提升一致的模式。对木质部和土壤水δD值的同步分析表明,10种代表性木本植物(5种落叶植物和5种常绿植物)之间存在明显的水资源分配差异。在这些物种中,4种常绿植物和1种落叶植物主要从上层土壤层(200厘米以上)获取水分,而3种落叶植物和1种常绿植物利用深层土壤水源(200厘米以下)。一种落叶植物表现出中间行为。每日总液流与木质部汁液δD值呈负相关,这表明在旱季用水速率较高的物种往往依赖更深层的土壤水源。在常绿物种中,最低叶片水势也与木质部水δD值呈负相关,这表明在更深层获取更容易获得的水分有助于维持更有利的植物水分状况。在两种常绿物种中,未观察到木质部水δD与植物大小之间的显著关系,这表明小型植物快速发育深根系存在很强的选择压力。土壤水分分配、叶片物候和叶片寿命的变化程度与塞拉多木本物种的高度多样性一致。

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