The contribution of natural and anthropogenic causes to soil acidification rates under different fertilization practices and site conditions in southern China.

IF 8.2 1区 环境科学与生态学 Q1 ENVIRONMENTAL SCIENCES Science of the Total Environment Pub Date : 2024-07-15 Epub Date: 2024-05-09 DOI:10.1016/j.scitotenv.2024.172986
Xingjuan Zhu, Gerard H Ros, Minggang Xu, Donghao Xu, Zejiang Cai, Nan Sun, Yinghua Duan, Wim de Vries
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Abstract

Excessive application of mineral fertilizers has accelerated soil acidification in China, affecting crop production when the pH drops below a critical value. However, the contributions of natural soil acidification, induced by leaching of bicarbonate, and anthropogenic causes of soil acidification, induced by nitrogen (N) transformations and removal of base cations over acid anions, are not well quantified. In this study, we quantified soil acidification rates, in equivalents (eq) of acidity, by assessing the inputs and outputs of all major cations and anions, including calcium, magnesium, potassium, sodium, ammonium, nitrate, bicarbonate, sulphate, phosphate and chloride, for 13 long-term experimental sites in southern China. The acidification rates strongly varied among fertilizer treatments and with the addition of animal manure. Bicarbonate leaching was the dominant acid production process in calcareous soils (23 keq ha-1 yr-1) and in non-calcareous paddy soils (9.6 keq ha-1 yr-1), accounting for 80 % and 68 % of the total acid production rate, respectively. The calcareous soils were strongly buffered, and acidification led no or a limited decline in pH. In contrast, N transformations were the most important driver for soil acidification at one site with upland crops on a non-calcareous soil, accounting for 72 % of total acid production rate of 8.4 keq ha-1 yr-1. In this soil, the soil pH considerably decreased being accompanied by a substantial decline in exchangeable base cation. Reducing the N surplus decreased the acidification rate with 10 to 54 eq per kg N surplus with the lowest value occurring in paddy soils and the highest in the upland soil. The use of manure, containing base cations, partly mitigated the acidifying impact of N fertilizer inputs and crop removal, but enhanced phosphorus (P) accumulation. Combining mineral fertilizer, manure and lime in integrative management strategies can mitigate soil acidification and minimize N and P losses.

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在中国南方不同施肥方式和场地条件下,自然和人为原因对土壤酸化率的影响。
在中国,过量施用矿物肥料加速了土壤酸化,当pH值低于临界值时就会影响作物产量。然而,由碳酸氢盐淋溶引起的自然土壤酸化,以及由氮(N)转化和碱式阳离子去除酸式阴离子引起的人为土壤酸化,其贡献还没有很好地量化。在这项研究中,我们通过评估中国南方 13 个长期实验点所有主要阳离子和阴离子(包括钙、镁、钾、钠、铵、硝酸盐、碳酸氢盐、硫酸盐、磷酸盐和氯化物)的输入和输出,以酸度当量(eq)为单位量化了土壤酸化率。不同肥料处理和添加动物粪便的酸化率差异很大。碳酸氢盐浸出是石灰性土壤(23 keq ha-1 yr-1)和非石灰性水稻土(9.6 keq ha-1 yr-1)的主要产酸过程,分别占总产酸率的 80% 和 68%。石灰性土壤具有很强的缓冲能力,酸化不会导致 pH 值下降或下降有限。与此相反,在一个非石灰性土壤上种植高地作物的地点,氮的转化是土壤酸化的最主要驱动因素,占总产酸量(8.4 千克/公顷-年-1)的 72%。在这种土壤中,土壤 pH 值显著下降,同时可交换碱式阳离子也大幅减少。减少氮过剩量可降低酸化率,每千克氮过剩量可降低 10 至 54 eq,其中水稻田土壤的酸化率最低,而高地土壤的酸化率最高。使用含有碱式阳离子的粪肥部分缓解了氮肥投入和作物移除对酸化的影响,但增加了磷(P)的积累。在综合管理策略中结合使用矿物肥料、粪肥和石灰可以缓解土壤酸化,最大限度地减少氮和磷的损失。
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来源期刊
Science of the Total Environment
Science of the Total Environment 环境科学-环境科学
CiteScore
17.60
自引率
10.20%
发文量
8726
审稿时长
2.4 months
期刊介绍: The Science of the Total Environment is an international journal dedicated to scientific research on the environment and its interaction with humanity. It covers a wide range of disciplines and seeks to publish innovative, hypothesis-driven, and impactful research that explores the entire environment, including the atmosphere, lithosphere, hydrosphere, biosphere, and anthroposphere. The journal's updated Aims & Scope emphasizes the importance of interdisciplinary environmental research with broad impact. Priority is given to studies that advance fundamental understanding and explore the interconnectedness of multiple environmental spheres. Field studies are preferred, while laboratory experiments must demonstrate significant methodological advancements or mechanistic insights with direct relevance to the environment.
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