[1]周学堂,段义字.退耕宜林区仁用杏林地土壤贮水特性分析[J].水土保持研究,2007,14(06):109-111.
ZHOU Xue-tang,DUAN Yi-zi.Analysis on Soil Water Retaining Properties of Almond-apricot Forest in Returning Farmland to Forest Area[J].Research of Soil and Water Conservation,2007,14(06):109-111.
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《水土保持研究》[ISSN:1005-3409/CN:61-1272/P]
卷:
14
期数:
2007年06期
页码:
109-111
栏目:
出版日期:
1900-01-01
- Title:
-
Analysis on Soil Water Retaining Properties of Almond-apricot Forest in Returning Farmland to Forest Area
- 作者:
-
周学堂1, 段义字2
-
1. 灵台县水土保持局, 甘肃 灵台 744400;
2. 平凉市水土保持科学研究所, 甘肃 平凉 744000
- Author(s):
-
ZHOU Xue-tang1, DUAN Yi-zi2
-
1. Soil and Water Conservation Bureau of Lingtai County, Lingtai, Gansu 744000, China;
2. Soil and Water Conservation Research Institute of Pingliang City, Pingliang, Gansu 744000, China
-
- 关键词:
-
退耕宜林区; 仁用杏林地; 土壤贮水; 土壤有效蓄水容量
- Keywords:
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returning farmland to forest; almond-apricot; soil water retaining; effective soil and water storing capacity
- 分类号:
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S715.3
- 摘要:
-
通过对平凉市退耕宜林区仁用杏林地、荒坡草地和农耕地3个地类土壤的孔隙分布及贮水特征等对照分析表明,仁用杏林地及荒草地土壤的蓄水容量较农耕地高,分别为农耕地的1.3和1.07倍,两者有效蓄水容量分别为农耕地的1.47和1.09倍;非毛管平均孔隙度为仁用杏林地(11.17%)>农耕地(10.99%)>荒草地(10.92%);仁用杏林地土壤水分的贮存能力最强,大于农耕地和荒草地,表明仁用杏在提高退耕地土壤入渗能力、减轻地表径流方面具有良好作用;仁用杏林地土壤水分的垂直变化梯度较大,从0-60 cm土层含水量的11.6%骤减为60-100 cm的9.7%,上下土层的贮水量94 mm/60 cm和61 mm/40 cm,下层土壤湿度明显小于上层。
- Abstract:
-
Through the comparison of soil pore distribution and water retaining properties of almond-apricot forest, grassland and farmland in Pingliang, the result shows that the soil water storing capacity of almond-apricot forest and grassland is 1.3 times and 1.07 times than that of farmland, the effective soil water storing capacity of both is 1.47 times and 1.09 times than that of farmland; Non-capillary porosity:almond-apricot (11.17%) >farmland (10.99%) >grassland (10.92%); The soil water storing capacity of almond-apricot forest is the strongest, which indicates that the almond apricot forest has good effect in increasing soil infiltration capacity and reducing surface runoff; the soil water of almond-apricot varied vertically, from 11.6% in 0-60 cm soil layer to 9.7% in 60-100 cm soil layer.The soil water storing capacity of upper and deep soil layer is 61 mm/40 cm and 94 mm/60 cm, the deep soil moisture is smaller than that of upper soil.
参考文献/References:
[1] 郑培龙, 肖江伟, 等.重庆缙云山典型林分林地土壤贮水特性研究[J].水土保持研究, 2006, 13 (2):195-197.
[2] 王孟本, 李洪建.柠条林土壤水分生态环境特征研究初报[J].中国科学院水利部西北水土保持研究所集刊, 1989 (10):155-169.
[3] 北京林学院.土壤学[M].北京:中国林业出版社, 1982:140-148.
[4] 段义字.堡子沟梁峁顶沙棘混交林生态经济效应研究[J].人民黄河, 1994, 16 (11):29-32.
更新日期/Last Update:
1900-01-01