阮长明, 王 猛, 孙永玉, 杜寿康, 唐国勇, 张春华, 欧朝蓉, 罗 孔. 金沙江流域干热河谷土壤肥力特征及其影响因素[J]. 土壤通报, 2024, 55(1): 93 − 101. DOI: 10.19336/j.cnki.trtb.2022092904
引用本文: 阮长明, 王 猛, 孙永玉, 杜寿康, 唐国勇, 张春华, 欧朝蓉, 罗 孔. 金沙江流域干热河谷土壤肥力特征及其影响因素[J]. 土壤通报, 2024, 55(1): 93 − 101. DOI: 10.19336/j.cnki.trtb.2022092904
RUAN Chang-ming, WANG Meng, SUN Yong-yu, DU Shou-kang, TANG Guo-yong, ZHANG Chun-hua, OU Chao-rong, LUO Kong. Characteristics of Soil Fertility and the Influencing Factors in the Hot-dry Valley of Jinsha River[J]. Chinese Journal of Soil Science, 2024, 55(1): 93 − 101. DOI: 10.19336/j.cnki.trtb.2022092904
Citation: RUAN Chang-ming, WANG Meng, SUN Yong-yu, DU Shou-kang, TANG Guo-yong, ZHANG Chun-hua, OU Chao-rong, LUO Kong. Characteristics of Soil Fertility and the Influencing Factors in the Hot-dry Valley of Jinsha River[J]. Chinese Journal of Soil Science, 2024, 55(1): 93 − 101. DOI: 10.19336/j.cnki.trtb.2022092904

金沙江流域干热河谷土壤肥力特征及其影响因素

Characteristics of Soil Fertility and the Influencing Factors in the Hot-dry Valley of Jinsha River

  • 摘要:
    目的 探明特殊生境土壤肥力的环境影响因子,为金沙江干热河谷植被恢复和生态治理提供基础和决策依据。
    方法 在金沙江干热河谷上、中、下游共设置47个样地,通过野外调查、土壤采集和室内分析,对比研究其表层土壤肥力特征及其环境影响因子。
    结果 ①金沙江干热河谷上、中、下游土壤肥力受气候、植被等环境因子影响,上游土壤肥力特征优于中、下游,中游土壤肥力状态最差;②金沙江干热河谷土壤肥力受植被类型的影响较大,其中天然林土壤孔隙度、有机质、全氮、全磷含量等显著(P < 0.05)高于稀树灌草丛,人工林土壤肥力在整体上也优于稀树灌草丛;③金沙江干热河谷海拔升高使环境温度降低、湿度增大、植被从稀树灌草丛向人工林和天然林逐渐过渡,导致土壤孔隙度和养分含量等土壤肥力特征随海拔升高而显著(P < 0.05)提升;④金沙江干热河谷受光照、水分等条件影响,阴坡土壤肥力状况优于阳坡。
    结论 金沙江干热河谷土壤肥力受不同区段、植被类型、海拔和坡向等环境因子的影响,其土壤肥力状态存在一定程度的区域差异。因此在金沙江干热河谷植被恢复和生态治理的实践中,应根据不同区段、植被类型、海拔、坡向等环境条件制定相应的植被恢复管理方案,这样才能获得更好的植被恢复效益。

     

    Abstract:
    Objective The purpose of this study is to investigate the environmental factors affecting soil fertility in special habitats, and to provide basis and decision-making basis for vegetation restoration and ecological management in the Dry-hot valley of Jinsha River.
    Method The surface soil fertility and their influencing factors were comparatively studied by field investigation, soil collection and laboratory analysis from 47 plots in the upper, middle and lower reaches in the Dry-hot valley of Jinsha River.
    Result ① The soil fertility in the upper, middle and lower reaches in the Dry-hot valley of Jinsha River was affected by climate, vegetation and other environmental factors. The soil fertility in the upper reaches was better than that in the middle and lower reaches, and the soil fertility in the middle reaches was the worst; ② The soil fertility in the Dry-hot valley of Jinsha River was significantly affected by vegetation types. The soil porosity, organic matter, total nitrogen and total phosphorus contents of natural forest were significantly (P < 0.05) higher than those of savannah, and the soil fertility of artificial forest was also better than that of savannah; ③The increase of altitude in the Dry-hot valley of Jinsha River resulted in the decrease of ambient temperature, the increase of humidity, the gradual transition of vegetation from savanna to artificial forest and natural forest, and the soil fertility characteristics such as soil porosity and nutrient content increased significantly (P < 0.05) with the increase of altitude; ④The Dry-hot valley of Jinsha River was affected by light and water, which resulted in better soil fertility in the shade slope than in the sunny slope.
    Conclusion The study showed that the soil fertility in the Dry-hot valley of Jinsha River was affected by environmental factors such as different sections, vegetation types, elevation and slope direction. There were regional differences in soil fertility. Therefore, the corresponding vegetation restoration management scheme should be formulated according to the environmental conditions such as different sections, vegetation types, elevations and slope direction in the practice of vegetation restoration and ecological management in the Dry-hot valley of Jinsha River, so as to obtain better vegetation restoration benefits.

     

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