Zhe Zhang , Zhiyao Wang , Shaoming Ye , Shengqiang Wang
{"title":"Dynamic changes of soil aggregate-associated phosphorus adsorption-desorption characteristics in a chronosequence of Chinese fir plantations","authors":"Zhe Zhang , Zhiyao Wang , Shaoming Ye , Shengqiang Wang","doi":"10.1016/j.still.2025.106479","DOIUrl":null,"url":null,"abstract":"<div><div>Successive cultivation of Chinese fir affects soil phosphorus (P) adsorption-desorption characteristics by altering both abiotic and biotic factors, such as soil aggregate size and microbial activities. However, previous studies have predominantly focused on individual factors (abiotic or biotic factors) without considering their combined effects on soil P adsorption-desorption characteristics. To address the research gaps, this study was conducted to investigate the response of abiotic factors (P forms, soil organic matters (SOM), iron and aluminum oxides (Fe<sub>2</sub>O<sub>3</sub> and Al<sub>2</sub>O<sub>3</sub>) concentrations, and aggregate sizes) and biotic factors (microbial activities) to Chinese fir stand ages (control, 9-yr, 17-yr, and 26-yr) and how the combined relationship affect P adsorption-desorption characteristics in Chinese fir plantations. The results showed that under the same initial P concentration (0.0, 0.3, 1.5, 3.0, 10.0, 20.0, and 50.0 mg L<sup>−1</sup>), parameters of P adsorption-desorption characteristics including the quantity of stable adsorption P, quantity of stable desorption P, adsorption P rate, and desorption P rate in macro-aggregates (> 0.25 mm) were significantly higher than that in the micro-aggregates (< 0.25 mm). However, in 26-yr of Chinese fir plantations, parameters of P adsorption-desorption characteristics within almost all aggregate fractions significantly decreased, driven by declines in inorganic P, SOM, amorphous Fe<sub>2</sub>O<sub>3</sub> and Al<sub>2</sub>O<sub>3</sub>, macro-aggregates, and microbial biomass (as indicated by PLFAs). The order of factors affecting P adsorption-desorption characteristics variation is P forms, SOM, microbial biomass, and Fe<sub>2</sub>O<sub>3</sub> and Al<sub>2</sub>O<sub>3</sub>. The results of this study indicate crucial factors affecting the P adsorption-desorption process, with a combined effect of abiotic factors within the culture of Chinese fir. Therefore, to prevent significant soil P losses and promote P utilization efficiency, it is crucial to consider the combined impacts of abiotic and biotic factors on soil P cycling characteristics across different stand ages during Chinese fir cultivation.</div></div>","PeriodicalId":49503,"journal":{"name":"Soil & Tillage Research","volume":"249 ","pages":"Article 106479"},"PeriodicalIF":6.1000,"publicationDate":"2025-02-06","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/S0167198725000339","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}
引用次数: 0
Abstract
Successive cultivation of Chinese fir affects soil phosphorus (P) adsorption-desorption characteristics by altering both abiotic and biotic factors, such as soil aggregate size and microbial activities. However, previous studies have predominantly focused on individual factors (abiotic or biotic factors) without considering their combined effects on soil P adsorption-desorption characteristics. To address the research gaps, this study was conducted to investigate the response of abiotic factors (P forms, soil organic matters (SOM), iron and aluminum oxides (Fe2O3 and Al2O3) concentrations, and aggregate sizes) and biotic factors (microbial activities) to Chinese fir stand ages (control, 9-yr, 17-yr, and 26-yr) and how the combined relationship affect P adsorption-desorption characteristics in Chinese fir plantations. The results showed that under the same initial P concentration (0.0, 0.3, 1.5, 3.0, 10.0, 20.0, and 50.0 mg L−1), parameters of P adsorption-desorption characteristics including the quantity of stable adsorption P, quantity of stable desorption P, adsorption P rate, and desorption P rate in macro-aggregates (> 0.25 mm) were significantly higher than that in the micro-aggregates (< 0.25 mm). However, in 26-yr of Chinese fir plantations, parameters of P adsorption-desorption characteristics within almost all aggregate fractions significantly decreased, driven by declines in inorganic P, SOM, amorphous Fe2O3 and Al2O3, macro-aggregates, and microbial biomass (as indicated by PLFAs). The order of factors affecting P adsorption-desorption characteristics variation is P forms, SOM, microbial biomass, and Fe2O3 and Al2O3. The results of this study indicate crucial factors affecting the P adsorption-desorption process, with a combined effect of abiotic factors within the culture of Chinese fir. Therefore, to prevent significant soil P losses and promote P utilization efficiency, it is crucial to consider the combined impacts of abiotic and biotic factors on soil P cycling characteristics across different stand ages during Chinese fir cultivation.
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.