|Table of Contents|

Bidirectional Replenishment Characteristics and Evolution Process of Soil Nutrients in Mountainous Areas(PDF)

《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

Issue:
2025年第04期
Page:
780-793
Research Field:
黄河流域生态保护和高质量发展专刊(下)
Publishing date:

Info

Title:
Bidirectional Replenishment Characteristics and Evolution Process of Soil Nutrients in Mountainous Areas
Author(s):
SHI Bai-lei1; SHEN Yan-jun1; 2; 3*; PENG Jian-bing1; 2; 3; YUAN Yan-zhao1; NING Yi-bing1; 2; 3; CHEN Xing4; ZHU Jin-yu1; ZHANG Sheng-wei1; LI Si-rui1
(1. School of Geological Engineering and Geomatics, Chang'an University, Xi'an 710054, Shaanxi, China; 2. State Key Laboratory of Loess Science, Xi'an 710054, Shaanxi, China; 3. Academy of Yellow River Sciences of Shaanxi Province, Chang'an University, Xi'an 710054, Shaanxi, China; 4. College of Geology and Environment, Xi'an University of Science and Technology, Xi'an 710054, Shaanxi, China)
Keywords:
mountainous soil;  sequential structure;  nutrient replenishment;  geochemistry;  biological cycle;  control mechanism;  evolution process;  flux model
PACS:
S155.4+5
DOI:
10.19814/j.jese.2025.01028
Abstract:
Mountainous soil has a typical multi-layered sequence structure, which is a comprehensive product of bedrock weathering and atmosphere-earth's surface biological cycles, and the corresponding sources of soil nutrient also reflect the bidirectional replenishment characteristics of bedrock and earth's surface processes. In order to explore the coupling relationship between endogenous and exogenous replenishment of soil nutrients in mountainous areas, the replenishment mechanism of soil nutrients was systematically sorted out by bedrock geochemistry and earth's surface processes, the weathering differences of different lithologic minerals and the regulating and controlling effects of different earth's surface processes on soil nutrients in mountainous areas were discussed, and the synergistic relationships among material flow, energy transformation and ecological service functions were explained; finally, based on the spatio-temporal evolution process of bidirectional replenishment of soil nutrient, a soil nutrient flux model was established to reflect the bidirectional replenishment of bedrock weathering and atmosphere-earth's surface biological cycles at regional scale. The results show that ① the bedrock weathering affects vegetation growth by controlling nutrient availability, groundwater storage capacity, structural development degree and terrain shaping; ② the atmosphere-earth's surface biological cycle affects vegetation growth by regulating soil environment, nutrient form conversion and utilization frequency; ③ the difference drive in time and the superposition coupling in space of bedrock weathering and earth's surface processes together shape the complex and unique soil nutrient pattern in mountainous areas; ④ a nutrient flux model that considers bedrock weathering on a time scale is helpful to understand the nutrient demand strategies of ecosystems and the balance mechanism of eco-geological systems in regional mountainous areas. This study aims to provide a new understanding of the bidirectional sources of soil nutrients in mountainous areas, and suggests that attention should be paid to the effects of bedrock geochemistry on earth's surface ecosystems, which is of great significance for the scientific management of soil resources in mountainous areas and the realization of sustainable development of ecosystems.

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Last Update: 2025-07-25