Dynamic Variation of Sapwood Flow of Three Main Tree Species in a Soft Sand-rock Area[J]. 2017, 31(5): 203-207.
DOI:
Dynamic Variation of Sapwood Flow of Three Main Tree Species in a Soft Sand-rock Area[J]. 2017, 31(5): 203-207. DOI: 10.13870/j.cnki.stbcxb.2017.05.032.
Dynamic Variation of Sapwood Flow of Three Main Tree Species in a Soft Sand-rock Area
To understand the water use character of main tree species in soft sand-rock area
three main tree species (Caragana korshinskii Kom、Hippophae rhamnoides Linn. Pinus tabuliformis) in Geqiugou
Ordos
Inner Mongolia was examined using stem heart balance method to explore sap flow of these three tree species under different weather conditions and the daily change. The results showed: (1) The sap flow rates of the three tree species showed a unimodal curve
and nearly reached the peak at the same time during growing. (2) In the sunny day
the sapflow rate of Hippophae rhamnoides Linn was the highest
about 0.11772cm/s
the sap flow rate of Caragana korshinskii Kom and Pinus tabuliformis were similar; the daily average rates of the three species were 0.02901cm/s
0.01815cm/s
and 0.02203cm/s
respectively. (3) In different weather conditions
the sapflow rates of the three species showed sunny day>cloudy day>rainy day
and the time when they reached the peak showed sunny day>cloudy day>rainy day. The results of the study are to provide theoretical basis for studying the water supply-demand relationship of plants in soft sand-rock area and environmental management.
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Related Author
DING Fangjun
ZHAO Wenjun
HOU Yiju
CUI Yingchun
SHU Deyuan
LIU Yanhui
CHEN Yunming
QIAO Yuning
Related Institution
Guizhou Provincial Forestry Academy
College of Resources and Environment, Shanxi Agricultural University, Taigu
Institute of Soil and Water Conservation, Northwest Agriculture and Forestry University, Yangling
State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation, Chinese Academy of Sciences, Ministry of Water Resources, Yangling
Institute of Soil and Water Conservation, Chinese Academy of Sciences and Ministry of Water Resources, Yangling