Soil phosphorus cycling in greenhouse vegetable production system: New insights from phosphate oxygen isotope

IF 6 1区 农林科学 Q1 AGRICULTURE, MULTIDISCIPLINARY
Tiantian Zhao , Kang Tian , Benle Liu , Wenyou Hu , Biao Huang , Yongcun Zhao
{"title":"Soil phosphorus cycling in greenhouse vegetable production system: New insights from phosphate oxygen isotope","authors":"Tiantian Zhao ,&nbsp;Kang Tian ,&nbsp;Benle Liu ,&nbsp;Wenyou Hu ,&nbsp;Biao Huang ,&nbsp;Yongcun Zhao","doi":"10.1016/j.agee.2024.109286","DOIUrl":null,"url":null,"abstract":"<div><p>Phosphorus (P) accumulation in soils of the greenhouse vegetable production (GVP) system is common due to intensive fertilization. However, the mechanism of P cycling in soils containing high P concentrations is not clear. In order to clarify the P cycling in GVP, 10 topsoils (0<img>30 cm) and 10 subsoils (30<img>60 cm) were sampled under two types of greenhouses (solar greenhouse and plastic greenhouse) in Shouguang, a typical GVP region of China. The pools of soil inorganic P following Hedley sequential extraction, and the oxygen isotopic composition of NaHCO<sub>3</sub> extracted phosphate (<em>δ</em><sup>18</sup>O<sub>NaHCO<span>3</span>_Pi</sub>) and HCl extracted phosphate (<em>δ</em><sup>18</sup>O<sub>HCl_Pi</sub>) were measured. Results showed that P in GVP, particularly in the solar greenhouse soils, accumulated significantly both in topsoil and subsoil. The main inorganic P pool in GVP soils was the HCl extracted, accounting for 50.26 %<img>72.76 % in topsoil and 44.42 %<img>57.89 % in subsoil, respectively. Values of <em>δ</em><sup>18</sup>O<sub>NaHCO<span>3</span>_Pi</sub> in most topsoil samples were within the isotopic equilibrium range (13.63 ‰<img>17.14 ‰). Values of soil <em>δ</em><sup>18</sup>O<sub>HCl_Pi</sub> in GVP, significantly higher than that in open field (11.41 ‰ in topsoil and 10.27 ‰ in subsoil), indicated more intensive P biological cycling and more secondary minerals formation altered the original characteristics of <em>δ</em><sup>18</sup>O<sub>HCl_Pi</sub> in GVP soil. The significant positive correlation of <em>δ</em><sup>18</sup>O<sub>NaHCO<span>3</span>_Pi</sub> values between topsoil and subsoil implied that the labile P<sub>i</sub> in subsoil was mainly influenced by its corresponding topsoil. Partially labile P, without biological cycling after fertilization of the topsoil, quickly migrated to the subsoil causing the P accumulation in the subsoil. The higher values of <em>δ</em><sup>18</sup>O<sub>NaHCO<span>3</span>_Pi</sub> and <em>δ</em><sup>18</sup>O<sub>HCl_Pi</sub> in solar greenhouse than plastic greenhouse suggested higher degree of P biological cycling, which were determined by the nutrient status. Overall, the phosphate oxygen isotope technology provides a deeper understanding of soil P cycling in GVP.</p></div>","PeriodicalId":7512,"journal":{"name":"Agriculture, Ecosystems & Environment","volume":"378 ","pages":"Article 109286"},"PeriodicalIF":6.0000,"publicationDate":"2024-09-07","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Agriculture, Ecosystems & Environment","FirstCategoryId":"97","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0167880924004043","RegionNum":1,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"AGRICULTURE, MULTIDISCIPLINARY","Score":null,"Total":0}
引用次数: 0

Abstract

Phosphorus (P) accumulation in soils of the greenhouse vegetable production (GVP) system is common due to intensive fertilization. However, the mechanism of P cycling in soils containing high P concentrations is not clear. In order to clarify the P cycling in GVP, 10 topsoils (030 cm) and 10 subsoils (3060 cm) were sampled under two types of greenhouses (solar greenhouse and plastic greenhouse) in Shouguang, a typical GVP region of China. The pools of soil inorganic P following Hedley sequential extraction, and the oxygen isotopic composition of NaHCO3 extracted phosphate (δ18ONaHCO3_Pi) and HCl extracted phosphate (δ18OHCl_Pi) were measured. Results showed that P in GVP, particularly in the solar greenhouse soils, accumulated significantly both in topsoil and subsoil. The main inorganic P pool in GVP soils was the HCl extracted, accounting for 50.26 %72.76 % in topsoil and 44.42 %57.89 % in subsoil, respectively. Values of δ18ONaHCO3_Pi in most topsoil samples were within the isotopic equilibrium range (13.63 ‰17.14 ‰). Values of soil δ18OHCl_Pi in GVP, significantly higher than that in open field (11.41 ‰ in topsoil and 10.27 ‰ in subsoil), indicated more intensive P biological cycling and more secondary minerals formation altered the original characteristics of δ18OHCl_Pi in GVP soil. The significant positive correlation of δ18ONaHCO3_Pi values between topsoil and subsoil implied that the labile Pi in subsoil was mainly influenced by its corresponding topsoil. Partially labile P, without biological cycling after fertilization of the topsoil, quickly migrated to the subsoil causing the P accumulation in the subsoil. The higher values of δ18ONaHCO3_Pi and δ18OHCl_Pi in solar greenhouse than plastic greenhouse suggested higher degree of P biological cycling, which were determined by the nutrient status. Overall, the phosphate oxygen isotope technology provides a deeper understanding of soil P cycling in GVP.

温室蔬菜生产系统中的土壤磷循环:磷氧同位素的新发现
由于大量施肥,温室蔬菜生产(GVP)系统的土壤中普遍存在磷积累现象。然而,高浓度磷土壤中的磷循环机制尚不清楚。为了弄清温室蔬菜生产中的磷循环,研究人员在中国典型的温室蔬菜生产地区寿光的两种温室(日光温室和塑料大棚)下采集了 10 个表层土(030 厘米)和 10 个底层土(3060 厘米)的样本。测定了土壤中无机磷的海德力顺序提取池,以及 NaHCO3 提取磷酸盐(δ18ONaHCO3_Pi)和盐酸提取磷酸盐(δ18OHCl_Pi)的氧同位素组成。结果表明,龙胆紫中的磷,尤其是日光温室土壤中的磷,在表土和底土中都有显著积累。盐酸提取物是龙胆紫土壤中主要的无机钾库,分别占表土和底土的 50.26 % 和 72.76 % 和 44.42 % 和 57.89 %。大多数表层土样本中的δ18ONaHCO3_Pi 值都在同位素平衡范围内(13.63 ‰17.14 ‰)。龙湾洼地土壤 δ18OHCl_Pi 的值明显高于露地(表土 11.41 ‰,底土 10.27 ‰),这表明龙湾洼地土壤中更密集的钾生物循环和更多的次生矿物形成改变了 δ18OHCl_Pi 的原有特征。表土与底土的δ18ONaHCO3_Pi 值呈明显的正相关,这意味着底土中的可移动钙主要受其相应表土的影响。表层土壤施肥后,部分可迁移态 P 未经生物循环,迅速迁移到底层土壤,导致 P 在底层土壤中积累。日光温室中的δ18ONaHCO3_Pi 和δ18OHCl_Pi 值高于塑料大棚,这表明磷的生物循环程度较高,这是由养分状况决定的。总之,磷氧同位素技术有助于更深入地了解龙江植物园土壤中的磷循环。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
求助全文
约1分钟内获得全文 求助全文
来源期刊
Agriculture, Ecosystems & Environment
Agriculture, Ecosystems & Environment 环境科学-环境科学
CiteScore
11.70
自引率
9.10%
发文量
392
审稿时长
26 days
期刊介绍: Agriculture, Ecosystems and Environment publishes scientific articles dealing with the interface between agroecosystems and the natural environment, specifically how agriculture influences the environment and how changes in that environment impact agroecosystems. Preference is given to papers from experimental and observational research at the field, system or landscape level, from studies that enhance our understanding of processes using data-based biophysical modelling, and papers that bridge scientific disciplines and integrate knowledge. All papers should be placed in an international or wide comparative context.
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术官方微信