摘要
在青藏高原东部的一个季节性高山雪场,沿着融雪梯度设置三个梯度部位,在每个部位测量融雪时间及土壤水分等因子,并测定长毛风毛菊(Saussurea hieracioides Hook.F.)的单株叶数、单叶面积和地上生物量等个体生长特征.结果表明,晚融部位的生长季长度比早融部位迟了将近一个月,晚融部位的土壤水分含量比早融部位高,在早融到晚融的梯度上长毛风毛菊的个体生长逐渐增加;长毛风毛菊个体特征的变化与融雪时间的早晚相反而与土壤含水量高低一致.
In a seasonal alpine snow field in the east of Qinghai - Tibet Plateau, three portions were estab- lished along snowmeh gradient. At each portion, snowmelt time, soil moisture and individual growth (including leaves per individual, area per leaf and aboveground biomass) of Saussurea Hieracioides Hook. F. were measured. The results showed that the length of growing season at late - melting portion was nearly one month later than that at early - melting portion. However, soil moisture at late - melting portion was higher than that at early - melting portion. In addition, individual growth gradually increased from early - to late - melting portion. The results suggested that individual growth of this species was reverse to snowmeh timing, whereas it was consistent with soil moisture.
出处
《重庆文理学院学报(自然科学版)》
2009年第1期5-8,共4页
Journal of Chongqing University of Arts and Sciences
基金
国家自然科学基金(40671181
30870396)
中国科学院项目(KZCX2-YW-418
KZCX2-XB2-02)
国家科技部项目(2006BAC01A15
2006BAC01A11)
关键词
青藏高原东部
融雪时间
土壤含水量
个体生长
长毛风毛菊
East of Qinghai - Tibean Plateau
snowmeh time
soil moisture
individual growth
Saussurea Hieracioides Hook. F