欢迎访问《应用生态学报》官方网站,今天是 分享到:

应用生态学报 ›› 2017, Vol. 28 ›› Issue (7): 2155-2163.doi: 10.13287/j.1001-9332.201707.011

• • 上一篇    下一篇

北京山区侧柏-荆条系统水分来源对降雨事件的响应

赵娜1, 孟平2, 何雅冰1, 娄源海1, 余新晓1*   

  1. 1北京林业大学水土保持学院, 水土保持与荒漠化防治教育部重点实验室, 北京 100083
    2中国林业科学研究院林业研究所, 国家林业局林木培育重点实验室, 北京 100091
  • 收稿日期:2016-11-07 修回日期:2017-04-07 发布日期:2017-07-18
  • 通讯作者: *mail:yuxinxiao0707@126.com
  • 作者简介:赵娜,女,1985年生,博士.主要从事森林生态学、稳定同位素生态学研究.E-mail:zhaona1019@126.com
  • 基金资助:
    本文由国家自然科学基金项目(41430747)和北京市教委项目(CEFF-PXM2016_014207_000038)资助

Response of water sources in Platycladus orientalis and Vitex negundo var heterophylla system to precipitation events in mountain area of Beijing, China

ZHAO Na1, MENG Ping2, HE Ya-bing1, LOU Yuan-hai1, YU Xin-xiao1*   

  1. 1Ministry of Education Key Laboratory of Soil and Water Conversation and Desertification Combating, College of Soil and Water Conservation, Beijing Forestry University, Beijing 100083, China
    2State Forestry Administration Key Laboratory of Tree Breeding and Cultivation, Research Institute of Forestry, Chinese Academy of Forestry, Beijing 100091, China
  • Received:2016-11-07 Revised:2017-04-07 Published:2017-07-18
  • Contact: *mail:yuxinxiao0707@126.com
  • Supported by:
    This work was supported by the National Natural Science Foundation of China (41430747) and the Beijing Municipal Education Commission (CEFF-PXM2016_014207_000038).

摘要: 分析了北京鹫峰山区侧柏、荆条枝条水及其潜在水分来源的氢氧同位素特征,运用IsoSource模型解析侧柏、荆条系统水分利用来源的季节变化及其对降雨事件的响应.结果表明:旱季初期(4月)研究区0~20 cm土层富集土壤水18O值,20 cm以下该值则随着土层深度增加逐渐减小,侧柏主要利用前2~3 d降雨补充的0~30 cm层土壤水;旱季末期(6月)侧柏和荆条分别利用当天雨水补充的0~10和10~30 cm层土壤水;雨季(7月)侧柏利用前期降水补给的0~40 cm层土壤水(59.3%)和近期降水(12.5%),荆条则利用近期降雨供给的0~30 cm层土壤水;侧柏的土壤水分来源逐月加深,至生长季末(11月)其主要利用60~80 cm层土壤水(前2~3 d降雨补给),而荆条枝条水δ18O值远离各水分来源δ18O值.两物种对水分的竞争压力小,适应本区域气候特征,尤其在应对特大暴雨等极端天气时,植物系统垂直分布的水分来源能够有效分流洪峰,减小暴雨瞬时破坏力.

Abstract: This study aimed to qualify the potential water sources and their responses to seasonal precipitations for the system of Platycladus orientalis and Vitex negundo var. heterophylla by IsoSource model based on stable hydrogen and oxygen isotopic analysis in Jiufeng Mountain area of Beijing. The results showed that the 18O of water from 0-20 cm soil layer was enriched, whereas that was depleted as the soil layer deepened. P. orientalis used water mainly from 0-30 cm soil la-yer, being composed of rainwater 2-3 days before at the beginning of dry season. The water absorbed by P. orientalis and V. negundo sourced from 0-10 cm and 10-30 cm soil layer, which was fed on recent rainwater at the end of dry season. In wet season P. orientalis mainly accessed the soil water (from 0-40 cm layer, 59.3%) and recent rainwater (12.5%), while V. negundo drank the water from 0-30 cm soil layer derived from recent heavy rain. P. orientalis actively uptook the deeper soil water with time, until the end of growing season (November), its available water was from 60-80 cm soil layer and sourced from the rainwater happened 2-3 days before. Meanwhile, V. negundo completed its growing cycle and was on the brink of death. This system faced less competition for water use, stating its vertical water availability for climate adaptation in this region, which could reduce water and soil loss and minimize the instantaneous damage under heavy rainstorm attack.