金沙江下游乌东德和白鹤滩库区土壤养分空间分异特征
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国家自然科学基金项目(U2102209);自然资源部自然资源要素耦合过程与效应重点实验室开放课题(2024KFKT002);自然资源综合调查指挥中心科技创新课题(KC20230019);地质调查项目(DD20220888)


Soil nutrient heterogeneity at Wudongde and Baihetan reservoirs in the Jinsha river's lower reaches
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    摘要:

    干热河谷库区土壤养分的维持对水土保持和生态修复具有关键作用,但在库区不同位置的土壤养分特征尚不明确。研究以金沙江下游的乌东德和白鹤滩库区为案例,于库首、库中和库尾,按表层(0-10 cm)和次表层(10-20 cm)分层采集表层土壤样品,测定土壤养分含量。基于第二次土壤养分分级标准,集成模糊综合评价、随机森林模型和自然断点分析方法,构建土壤养分空间分异特征分析模型,厘清土壤养分空间分异特征,并提出分区管理策略。结果表明:(1)研究区土壤呈弱碱性,土壤有机质、全钾、速效钾、有效锰和有效铜含量较高,处于1级,有效锌含量为2级,阳离子交换量、有效硼和有效钼含量较低,处于4级,全磷处于5级;(2)0-10 cm土层土壤养分整体较高,处在0.53-0.66范围内,高值出现在乌东德和白鹤滩的库尾区,10-20 cm土层土壤养分整体处于0.43-0.58之间,其中土壤养分指数高值则出现在水电站的库中区。(3)表层土壤主要受人为活动和植被影响,次表层则更多受地形和土壤属性影响,库首大部分区域处在土壤养分保持区,库中总体为养分恢复区,库尾则是风险防控区,对于库尾应更多考虑增加植被种植,控制社会经济发展和人口增长带来的负面影响。研究通过系统构建可比的综合指标,能够分析梯级水电库区表层土壤养分的空间异质性,以实现上下游库区的综合管理,指示干热河谷地区的生态修复策略。

    Abstract:

    For the purpose of conserving soil and water as well as restore ecosystems, maintaining soil nutrient levels in dry-hot valley reservoir regions is essential. However, the spatial characteristics of soil nutrients within reservoir areas remain poorly understood. This study focused on the Wudongde and Baihetan reservoir areas located in the lower reaches of the Jinsha River. Surface soil samples were collected from the head, middle, and tail of the reservoir, including both surface layer (0-10 cm) and subsurface layer (10-20 cm), and the soil nutrient content were measured. Based on the second soil nutrient grading standard, a soil nutrient spatial differentiation analysis model was developed by integrating fuzzy comprehensive evaluation, the random forest model, and natural breakpoint analysis. This model aimed to elucidate the spatial differentiation characteristics of soil nutrients and propose zoning management strategies. The findings indicate that: (1) the soil in the study area was weakly alkaline, with high contents of soil organic matter, total potassium, available potassium, available manganese, and available copper, all of which were at level 1. Available zinc content was at level 2, while cation exchange capacity, available boron, and available molybdenum contents were low, at level 4, and total phosphorus was at level 5; (2) the nutrient in the 0-10 cm soil layer is generally high, ranging from 0.53 to 0.66; the highest values were found in the reservoir tail areas of Wudongde and Baihetan; for the 10-20 cm soil layer, the nutrient content generally ranges between 0.43 and 0.58, with the highest values located in the middle sections of the reservoirs; (3) Surface soil nutrient variation was mainly influenced by human activities and vegetation, whereas the subsurface soil was more affected by topography and soil properties. Most areas of the reservoir head were in the soil nutrient conservation zone, the reservoir middle was generally in the nutrient recovery zone, and the reservoir tail was in the risk prevention and control zone.

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廖丹琦,张连凯,杨万涛,张亚,李强,刘朋雨,王杰,宋琳,兰明国.金沙江下游乌东德和白鹤滩库区土壤养分空间分异特征.生态学报,2025,45(11):5124~5136

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