1. 内蒙古农业大学 沙漠治理学院,内蒙古,呼和浩特,010010
2. 内蒙古水利水电勘测设计院,内蒙古,呼和浩特,010020
3. 鄂尔多斯市林业和草原调查勘验中心,内蒙古,鄂尔多斯,017000
纸质出版:2022
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卜繁靖, 郭月峰, 祁伟, 等. 砒砂岩区三种沙棘根系特征与固土能力[J]. 水土保持通报, 2022,42(5):41-48.
Bu Fanjing, Guo Yuefeng, Qi Wei, et al. Root System Characteristics and Soil Consolidation Ability of Three Hippophae Rhamnoides Species in Feldspathic Sandstone Area[J]. Bulletin of Soiland Water Conservation, 2022, 42(5): 41-48.
卜繁靖, 郭月峰, 祁伟, 等. 砒砂岩区三种沙棘根系特征与固土能力[J]. 水土保持通报, 2022,42(5):41-48. DOI: 10.13961/j.cnki.stbctb.20220525.001.
Bu Fanjing, Guo Yuefeng, Qi Wei, et al. Root System Characteristics and Soil Consolidation Ability of Three Hippophae Rhamnoides Species in Feldspathic Sandstone Area[J]. Bulletin of Soiland Water Conservation, 2022, 42(5): 41-48. DOI: 10.13961/j.cnki.stbctb.20220525.001.
[目的] 研究中国沙棘(Hippophae rhamnoides ssp.sinensis)、太阳沙棘(Hippophae rhamnoides ssp.taiyang)、乌兰沙林沙棘(Hippophae rhamnoides ssp.mongolica “Wulanshalin”)在砒砂岩区的根系分布特征及林下土壤抗蚀性特征,为改善当地生态环境提供新的树种选择。[方法] 在野外挖土壤剖面获取根土复合体,在室内进行根扫描及崩解试验。[结果] ①沙棘根系垂直分布规律大致相似。随土层深度的增加,根长、根体积逐步减少。根系主要分布在0—60 cm土层,占总根量比例分别为90.96%(中国沙棘),83.38%(太阳沙棘),74.93%(乌兰沙林沙棘);粗根主要分布在0—40 cm土层。水平方向粗根主要分布在距根基0—20 cm的范围内,细根主要分布在20—100 cm范围内,且距根基越远细根含量越少,根系整体呈浅层化分布。②沙棘林下土壤崩解速度变化趋势基本一致。以0—20 cm表层土平均崩解速度最低。随着深度增加逐步增大,水平方向距根基部越远土壤平均崩解速度越大。土壤崩解速度表现为:中国沙棘(3.18 g/s)>太阳沙棘(1.27 g/s)>乌兰沙林沙棘(1.21 g/s)。③土壤崩解速度与沙棘根系分布有显著相关关系。垂直方向上受到粗根和细根的共同影响,水平方向主要受到细根的影响,细根对固持水土的作用更大。[结论] 太阳沙棘的根系含量高于乌兰沙林沙棘,且根系分布特征和林下土壤崩解速度变化规律联系更密切,更适用于砒砂岩区的水土流失防治工作。
[Objective] The root distribution characteristics of Hippophae rhamnoides ssp. sinensis
Hippophae rhamnoides ssp. taiyang
and H. rhamnoides ssp. mongolica “Wulanshalin” in a feldspathic area
and the characteristics of soil erosion resistance under the forests were analyzed in order to provide new tree species options for improving the local ecological environment. [Methods] The soil profiles were excavated in the field to obtain the root-soil complexes
and the root scanning and disintegration test were performed indoors. [Results] ① The vertical distribution patterns of roots for the three seabuckthorn species were similar. Root length and root volume gradually decreased with increasing soil depth
and roots were mainly located in the 0—60 cm soil layer
accounting for 90.96% of the total root amount for H. rhamnoides ssp. sinensis
83.38% for H. rhamnoides ssp. taiyang
and 74.93% for H. rhamnoides ssp. mongolica “Wulanshalin”. Thick roots were mainly located in the 0—40 cm soil layer. The thick roots in the horizontal direction were mainly located in the range of 0—20 cm from the base of the plant
and the fine roots were mainly located in the range of 20—100 cm. The farther away from the base
the fewer the fine roots. The overall root system was distributed in a shallow layer. ② The change trend of soil disintegration rate under the H. rhamnoides forest was basically the same. The average disintegration rate of the surface soil at 0—20 cm was the lowest
and the rate gradually increased with increasing depth. In the horizontal direction
the farther away from the base of the plant
the greater the average disintegration rate of the soil. The soil disintegration rate followed the order of: H. rhamnoides ssp. sinensis (3.18 g/s)> H. rhamnoides ssp. taiyang (1.27 g/s)> H. rhamnoides ssp. mongolica “Wulanshalin” (1.21 g/s). ③ There was a significant correlation between soil disintegration rate and root distribution of seabuckthorn. In the vertical direction
it was affected by both coarse and fine roots
while in the horizontal direction
it was mainly affected by fine roots
which have a greater effect on soil and water retention. [Conclusion] The root content of H rhamnoides ssp. taiyang was higher than that of H rhamnoides ssp. mongolica “Wulanshalin”
and the root distribution characteristics were more closely related to the change law of soil disintegration rate under the forest
which is more suitable for soil erosion prevention and control in the soft sandstone area.
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