Hydrological functions of several vegetations in Diediegou valley in north Liupan Mountain
View Fulltext  View/Add Comment  Download reader
  
DOI:10.7606/j.issn.1000-7601.2013.04.036
Key Words: Larix principis-rupprechtii  Hippophae rhamnoides  Ostryopsis davidiana  grassland  canopy interception  water holding capacity  soil physical property
Author NameAffiliation
LIU Qian1,2, WANG Ping1, XIONG Wei2, WANG Yan-hui2, DU A-peng3, LI Zhen-hua2, WANG Yan-bing4 (1.甘肃农业大学资源与环境学院 甘肃 兰州 7300702.中国林业科学研究院森林生态环境与保护研究所国家林业局森林生态环境重点实验室 北京 1000913.国家林业局桉树研究开发中心 广东 湛江 524022 4.内蒙古农业大学林学院 内蒙古 呼和浩特 010019) 
Hits: 1657
Download times: 1248
Abstract:
      The hydrological functions, in terms of canopy interception and water holding capacity of litters and soil layers, were assessed in several vegetations in the semi-arid region in north part of Liupan Mountain, Ningxia, China. The results indicated that the canopy interception differed notably among different vegetations, with the maximal value (24.80%) in the shrubs of Hippophae rhamnoides, followed by the plantations of Larix principis-rupprechtii(21.40%), and the minimal value (9.25%) in the shrubs of Ostryopsis davidiana. Conversely, the maximal stem flow ratio (33.1%) appeared in the shrubs of Ostryopsis davidiana, which exceeded the general range (2%~10%) of most shrubs in arid and semi-arid regions. From the aspect of seasonal variation, the maximal interception ratio appeared in June, then decreased from July to September, and increased again in October. However, the maximal interception amount appeared in July for all vegetations studied. The highest water holding capacity of litter layers was in the plantations of Larix principis-rupprec htii, followed by the shrubs of Ostryopsis davidiana and Hippophae rhamnoides and the grassland, being the same as the sequence of litter stock. The soil bulk density in 0~100 cm layer was minimal in the shrubs of Ostryopsis davidiana, and maximal in the shrubs of Hippophae rhamnoides. The total porosity and water-holding capacity were maximal in the plantations of Larix principis-rupprechtii, while the capillary porosity and capillary water-holding capa city were maximal in the shrubs of Ostryopsis davidiana, and the non-capillary porosity was maximal in the grassland; the worst soil porosities was found in the shrubs of Hippophae rhamnoides. Considering comprehensively the canopy interception, water holding capacity of litters and soil physical properties, the best hydrological functions appeared in the plantations of Larix principis-rupprechtii, then the shrubs of Ostryopsis davidiana and the grassland, and the worst functions appeared in the shrubs of Hippophae rhamnoides.