Qinqing Yang , Peng Wang , Jingyao Xiao , Shenghao Ai , Jianing Kou , Tingting Chen , Xiaoyan Ai , Jinqiang Ma , Yingwei Ai
{"title":"不同恢复方式对高寒矿山边坡土壤团聚体磷有效性和组分的影响","authors":"Qinqing Yang , Peng Wang , Jingyao Xiao , Shenghao Ai , Jianing Kou , Tingting Chen , Xiaoyan Ai , Jinqiang Ma , Yingwei Ai","doi":"10.1016/j.still.2025.106657","DOIUrl":null,"url":null,"abstract":"<div><div>The deficiency of soil phosphorus (P) resources is a challenge of worldwide concern. The efficiency of soil P utilization in alpine mine slopes is especially poor, which limits the growth of plants, making slopes difficult to restore and causing frequent natural disasters. In this study, three mine slopes were chosen as representative study sites on China's Qinghai-Tibet Plateau, and the soil aggregate P fractions' distribution and changes under frame beam restoration slope (FRS), metal wire mesh restoration slope (MRS), and natural slope (NS) were investigated, as well as the mechanisms relating P fractions to P availability. The results demonstrated that soil aggregate P availability and fractions in alpine mine slopes were significantly impacted by various restoration methods. In soil aggregates of both FRS and MRS, TP and AP contents were lower than NS, and showing a trend of FRS>MRS. The P activation coefficients were almost all < 2 % in the soil aggregates of three slopes, indicating that TP was difficult to convert to AP. In all three slopes, the total inorganic P contents of soil aggregates with varying particle sizes were NS > FRS > MRS. Classifying the P fractions by stability, the soil P fractions contents generally showed that active P < moderately active P < stable P, and soil aggregates with different particle sizes in FRS had substantially greater active P contents than those in MRS. Additionally, H<sub>2</sub>O-Pi and DHCl-Pi showed significant direct negative effects on AP, with path coefficients of −0.24 and −0.30 respectively. The physicochemical factors pH and SOM, which mainly drove changes in soil P fractions, also differed because they were affected by different restoration methods. This study will be dedicated to providing a theoretical framework for managing soil P in alpine mine slopes during the ecological restoration process and providing reference opinions for the selection of restoration techniques for alpine mines.</div></div>","PeriodicalId":49503,"journal":{"name":"Soil & Tillage Research","volume":"253 ","pages":"Article 106657"},"PeriodicalIF":6.1000,"publicationDate":"2025-05-16","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Effects of different restoration methods on soil aggregate phosphorus availability and fractions in alpine mine slopes\",\"authors\":\"Qinqing Yang , Peng Wang , Jingyao Xiao , Shenghao Ai , Jianing Kou , Tingting Chen , Xiaoyan Ai , Jinqiang Ma , Yingwei Ai\",\"doi\":\"10.1016/j.still.2025.106657\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>The deficiency of soil phosphorus (P) resources is a challenge of worldwide concern. The efficiency of soil P utilization in alpine mine slopes is especially poor, which limits the growth of plants, making slopes difficult to restore and causing frequent natural disasters. In this study, three mine slopes were chosen as representative study sites on China's Qinghai-Tibet Plateau, and the soil aggregate P fractions' distribution and changes under frame beam restoration slope (FRS), metal wire mesh restoration slope (MRS), and natural slope (NS) were investigated, as well as the mechanisms relating P fractions to P availability. The results demonstrated that soil aggregate P availability and fractions in alpine mine slopes were significantly impacted by various restoration methods. In soil aggregates of both FRS and MRS, TP and AP contents were lower than NS, and showing a trend of FRS>MRS. The P activation coefficients were almost all < 2 % in the soil aggregates of three slopes, indicating that TP was difficult to convert to AP. In all three slopes, the total inorganic P contents of soil aggregates with varying particle sizes were NS > FRS > MRS. Classifying the P fractions by stability, the soil P fractions contents generally showed that active P < moderately active P < stable P, and soil aggregates with different particle sizes in FRS had substantially greater active P contents than those in MRS. Additionally, H<sub>2</sub>O-Pi and DHCl-Pi showed significant direct negative effects on AP, with path coefficients of −0.24 and −0.30 respectively. The physicochemical factors pH and SOM, which mainly drove changes in soil P fractions, also differed because they were affected by different restoration methods. This study will be dedicated to providing a theoretical framework for managing soil P in alpine mine slopes during the ecological restoration process and providing reference opinions for the selection of restoration techniques for alpine mines.</div></div>\",\"PeriodicalId\":49503,\"journal\":{\"name\":\"Soil & Tillage Research\",\"volume\":\"253 \",\"pages\":\"Article 106657\"},\"PeriodicalIF\":6.1000,\"publicationDate\":\"2025-05-16\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Soil & Tillage Research\",\"FirstCategoryId\":\"97\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S0167198725002119\",\"RegionNum\":1,\"RegionCategory\":\"农林科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"SOIL SCIENCE\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Soil & Tillage Research","FirstCategoryId":"97","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0167198725002119","RegionNum":1,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"SOIL SCIENCE","Score":null,"Total":0}
Effects of different restoration methods on soil aggregate phosphorus availability and fractions in alpine mine slopes
The deficiency of soil phosphorus (P) resources is a challenge of worldwide concern. The efficiency of soil P utilization in alpine mine slopes is especially poor, which limits the growth of plants, making slopes difficult to restore and causing frequent natural disasters. In this study, three mine slopes were chosen as representative study sites on China's Qinghai-Tibet Plateau, and the soil aggregate P fractions' distribution and changes under frame beam restoration slope (FRS), metal wire mesh restoration slope (MRS), and natural slope (NS) were investigated, as well as the mechanisms relating P fractions to P availability. The results demonstrated that soil aggregate P availability and fractions in alpine mine slopes were significantly impacted by various restoration methods. In soil aggregates of both FRS and MRS, TP and AP contents were lower than NS, and showing a trend of FRS>MRS. The P activation coefficients were almost all < 2 % in the soil aggregates of three slopes, indicating that TP was difficult to convert to AP. In all three slopes, the total inorganic P contents of soil aggregates with varying particle sizes were NS > FRS > MRS. Classifying the P fractions by stability, the soil P fractions contents generally showed that active P < moderately active P < stable P, and soil aggregates with different particle sizes in FRS had substantially greater active P contents than those in MRS. Additionally, H2O-Pi and DHCl-Pi showed significant direct negative effects on AP, with path coefficients of −0.24 and −0.30 respectively. The physicochemical factors pH and SOM, which mainly drove changes in soil P fractions, also differed because they were affected by different restoration methods. This study will be dedicated to providing a theoretical framework for managing soil P in alpine mine slopes during the ecological restoration process and providing reference opinions for the selection of restoration techniques for alpine mines.
期刊介绍:
Soil & Tillage Research examines the physical, chemical and biological changes in the soil caused by tillage and field traffic. Manuscripts will be considered on aspects of soil science, physics, technology, mechanization and applied engineering for a sustainable balance among productivity, environmental quality and profitability. The following are examples of suitable topics within the scope of the journal of Soil and Tillage Research:
The agricultural and biosystems engineering associated with tillage (including no-tillage, reduced-tillage and direct drilling), irrigation and drainage, crops and crop rotations, fertilization, rehabilitation of mine spoils and processes used to modify soils. Soil change effects on establishment and yield of crops, growth of plants and roots, structure and erosion of soil, cycling of carbon and nutrients, greenhouse gas emissions, leaching, runoff and other processes that affect environmental quality. Characterization or modeling of tillage and field traffic responses, soil, climate, or topographic effects, soil deformation processes, tillage tools, traction devices, energy requirements, economics, surface and subsurface water quality effects, tillage effects on weed, pest and disease control, and their interactions.