1. 北京林业大学水土保持学院水土保持与荒漠化防治教育部重点实验室,北京,100083
2. 榆林学院,陕西,榆林,719000
纸质出版:2014
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刘蕾蕾, 朱清科, 赵维军, 等. 陕北黄土区衰退沙棘人工林改良土壤的作用[J]. 水土保持通报, 2014,33(3):311-315.
LIU Lei-lei, ZHU Qing-ke, ZHAO Wei-jun, et al. Soil Improvement by Degrade Sea-buckthorn Forests in Loess Region of Northern Shaanxi Province[J]. Bulletin of Soiland Water Conservation, 2014, 33(3): 311-315.
刘蕾蕾, 朱清科, 赵维军, 等. 陕北黄土区衰退沙棘人工林改良土壤的作用[J]. 水土保持通报, 2014,33(3):311-315. DOI: 10.13961/j.cnki.stbctb.2014.03.061.
LIU Lei-lei, ZHU Qing-ke, ZHAO Wei-jun, et al. Soil Improvement by Degrade Sea-buckthorn Forests in Loess Region of Northern Shaanxi Province[J]. Bulletin of Soiland Water Conservation, 2014, 33(3): 311-315. DOI: 10.13961/j.cnki.stbctb.2014.03.061.
为研究衰退沙棘人工林对土壤的改良功能
对陕北黄土区衰退沙棘人工林分轻度、中度、重度3种衰退类型进行了研究。结果表明: (1) 3种衰退类型沙棘人工林0-60 cm土层土壤速效磷、速效钾含量较对照均有提高。(2) 轻度衰退沙棘人工林对40-60 cm土层土壤有效氮
0-20 cm速效磷含量有显著提高作用。对20-40 cm土层土壤有效氮含量有极显著提高作用(由14.23 mg/kg增至22.39 mg/kg)。中度衰退沙棘人工林对20-60 cm土壤有机质、有效氮有显著提高作用。重度衰退沙棘人工林对0-20 cm土壤全氮含量的提高作用显著低于对照坡面。(3) 3种衰退类型沙棘人工林对20-40 cm土层速效磷含量的作用表现为中度衰退沙棘人工林最大
其次是轻度衰退沙棘林。其他土层则表现为随着衰退程度加深
沙棘人工林对土壤改良作用减弱。
In order to investigate the soil improvement by degrade sea-buckthorn forest
soil properties in 0-60 cm soil layers under slightly
moderately and severely degrade sea-buckthorn forests were measured. (1) The concentrations of soil available P and K under the three degrade sea-buckthorn forests in 0-60 cm soil layers were larger than those under undisturbed slopes. (2) The increases were significant at the level of 0.05 for the concentrations of soil available N in 40-60 cm soil layer and soil available P in 0-20 cm soil layer under slightly degrade sea-buckthorn forest. The increase was significant(at the level of 0.01) for the concentration of soil available N in 20-40 cm soil layer under slightly degrade sea-buckthorn forest(The available N content increased from 14.23 to 22.39 mg/kg in 20-40 cm soil layer). The increases were also significant(at the level of 0.05) for the concentration of soil organic matter and soil available N in 20-60 cm soil layer under moderately degrade sea-buckthorn forest. Decrease was significant(at the level of 0.05) for the concentration of soil total N in 0-20 cm soil layer under severely degrade sea-buckthorn forest. (3) The increases of soil available P in 20-40 cm soil layer under the three degrade sea-buckthorn forests were in the following order: moderately degrade forest > slightly decayed forest > severely degrade forest. Soil available P in the 0-20 and 20-40 cm soil layers increased as the following order: slightly degrade forest > moderately degrade forest > severely degrade forest.
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