Urban tree root systems and their survival near houses analyzed using ground penetrating radar and sap flow techniques

被引:13
作者
Jan ermák
Jiri Hru ka
Milena Martinková
Alois Prax
机构
来源
Plant and Soil | 2000年 / 219卷
关键词
clay soils; ground penetrating radar; roots; sap flow; water consumption;
D O I
暂无
中图分类号
学科分类号
摘要
Root systems of two mature Field maple trees (Acer campestre L.) growing in both shaded and non-shaded sites, on clay soil in an urban environment, were analyzed by ground penetrating radar (GPR), light microscope and sap flow techniques. The ground surface above the root systems was covered by asphalt. However, a small piece of garden existed near the non-shaded tree, and root area of roots growing in this direction increased significantly, due to a presumed increase in available water and nutrients. However, no garden was present near the shaded tree, therefore roots remaining under the asphalt surface did not increase in area in any particular direction. Maximum rooting depth of shaded and exposed trees, as determined by GPR, was approximately 1.4 and 1.7 m, respectively. The trees utilized relatively large amounts of water for transpiration, i.e. 65–140 l per fine summer day and in average 10 m3 per growing season. However, transpiration expressed per root surface area (and/or whole root system enveloping area) was practically the same in both trees, i.e. 1 dm3 m-2 d-1 or almost 100 dm3 m-2 per growing season. These figures represented about 50% of potential evapotranspiration when considering projected crown areas. Increased transpiration under long-term high evaporation demands may cause occasional local drying of soil around roots, associated with soil shrinking in clay, which can be followed by serious damage to buildings.
引用
收藏
页码:103 / 116
页数:13
相关论文
共 40 条
[1]  
Biddle PG(1983)Patterns of soil drying and moisture deficit in the vicinity of trees on clay soils Fourth Geotechnique Symposium 23 107-126
[2]  
Cabibel B.(1994)Continuity of water transfer in the soil-root-trunk system The case of fruit trees 14 503-514
[3]  
Coutts MP(1989)Factors affecting the direction of growth of tree roots Ann. Sci. For. 46 277-287
[4]  
Carlson WC(1987)Cross-sectional area relationships in root systems of loblolly and shortleaf pine Can. J. For. Res. 17 556-558
[5]  
Harrington CA(1988)Effect of root severing treatments on loblolly pine Can. J. For. Res. 18 1376-1385
[6]  
Carlson WC(1980)Water potential and sap flow rate in adult trees with moist and dry soil as used for the assessment of the root system depth Biol. Plant (Praha) 22 34-41
[7]  
Harrington CA(1982)Sap flow rate and transpiration dynamics in the full-grown oak (Quercus robur L.) in floodplain forest exposed to seasonal floods as related to potential evapotranspiration and tree dimensions Biologia Plantarum 24 446-460
[8]  
Farnum P(1990)Scaling up transpiration data between trees, stands and watersheds Silva Carelica 15 101-120
[9]  
Hallgren SW(1983)The influence of vegetation on the swelling and shrinking of clays in the United States of America Fourth Geotechnique Symposium 23 159-163
[10]  
Čermák J(1999)Mapping of tree root systems by means of the ground penetrating radar Tree Physiology 19 125-130