Effects of halophyte Suaeda salsa continuous cropping on physical and chemical properties of saline soil under drip irrigation in arid regions

IF 6 1区 农林科学 Q1 AGRICULTURE, MULTIDISCIPLINARY Agriculture, Ecosystems & Environment Pub Date : 2024-05-17 DOI:10.1016/j.agee.2024.109076
Sihai Liu , Ning Wang , Dongze Li , Changyan Tian , Ke Zhang , Mingfang Hu , Haishan Niu , Zhenyong Zhao
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Abstract

Soil salinization causes the degradation of soil structure, which seriously affects the global agricultural production. Currently, planting halophytes to improve saline soil has been widely used. However, most of the experiments were short-term, and the effect of long-term continuous cropping of halophytes on soil is still uncertain. This study aimed to investigate the multi-year effect of continuous cropping of euhalophyte Suaeda salsa on soil physicochemical properties. The space-for-time substitution approach was used to compare changes in soil physicochemical indicators under 3-year, 5-year, and 7-year continuous cropping periods of Suaeda salsa under drip irrigation, with bareland(0-year) serving as the control. In the 0–20 cm soil layer, the soil moisture content increased from 10.76% to 11.72–14.92%; in the 0–40 cm soil layer, the average bulk density decreased from 1.61 g cm−3 to 1.45–1.46 g cm−3 (P < 0.05), the average total porosity increased from 40.54% to 45.63–46.82% (P < 0.05), the average content of soil water-stable macroaggregates rose from 2.38% to 3.07–7.42%, and the average clay particle content declined from 20.88% to 16.63–18.63%; in the 0–60 cm soil layer, the average total salt content decreased from 48.11 g kg−1 to 12.43–22.01 g kg−1, and the average soil organic matter(SOM) content decreased from 8.73 g kg−1 to 7.40–8.15 g kg−1; in the 0–100 cm soil layer, the average pH value increased from 7.33 to 7.38–7.75, and the average content of Ca2+, Mg2+, Na+, K+, SO42-, and Cl- all decreased, whereas the average HCO3- content increased from 0.16 g kg−1 to 0.25–0.29 g kg−1. After 7 years of continuous cropping, the mean weight diameter (MWD) of 0–40 cm soil layer increased by 19.01%, the sodium adsorption ratio (SAR) of 0–40 cm soil layer decreased by 53.57% (P < 0.05), and the soil hydro-chemical type of 0–100 cm soil layer changed from Cl--Na+·Ca2+ to Cl-·SO42--Na+·Ca2+. The salt accumulation in the aboveground part of Suaeda salsa accounted for only 1.85–4.36% of the annual desalination quantity in the 0–100 cm soil layer. The continuous cropping of Suaeda salsa improved the soil structure and promoted salt leaching, which was the main mechanism of soil salt reduction. The results showed continuous cropping of Suaeda salsa under drip irrigation in arid regions is an effective method to improve saline soil, providing a theoretical reference for long-term continuous cropping of halophytes to improve saline soil in arid regions.

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盐生植物 Suaeda salsa 连作对干旱地区滴灌条件下盐碱土理化性质的影响
土壤盐碱化导致土壤结构退化,严重影响全球农业生产。目前,种植盐生植物来改良盐碱土壤已得到广泛应用。然而,大多数实验都是短期的,长期连续种植卤叶植物对土壤的影响还不确定。本研究旨在探讨连作褐藻(Suaeda salsa)对土壤理化性质的多年影响。研究采用空间-时间替代法,以裸露地(0 年)为对照,比较了滴灌条件下连续种植 3 年、5 年和 7 年苏埃达莎莎的土壤理化指标变化。在 0-20 cm 土层中,土壤含水量从 10.76% 增加到 11.72-14.92%;在 0-40 cm 土层中,平均容重从 1.61 g cm-3 降低到 1.45-1.46 g cm-3 (P < 0.05),平均总孔隙度由 40.54% 增至 45.63-46.82%(P <;0.05),土壤水稳性大颗粒平均含量由 2.38% 增至 3.07-7.42%,粘粒平均含量由 20.88% 降至 16.63-18。63%;在 0-60 cm 土层中,平均全盐含量由 48.11 g kg-1 降至 12.43-22.01 g kg-1,平均土壤有机质(SOM)含量由 8.73 g kg-1 降至 7.40-8.在 0-100 厘米土层中,平均 pH 值从 7.33 升至 7.38-7.75,Ca2+、Mg2+、Na+、K+、SO42- 和 Cl- 的平均含量均有所下降,而 HCO3- 的平均含量则从 0.16 g kg-1 升至 0.25-0.29 g kg-1。连作7年后,0-40 cm土层的平均重量直径(MWD)增加了19.01%,0-40 cm土层的钠吸附比(SAR)降低了53.57%(P < 0.05),0-100 cm土层的土壤水化学类型由Cl--Na+-Ca2+转变为Cl--SO42--Na+-Ca2+。水飞蓟地上部分的盐分积累仅占 0-100 cm 土层年脱盐量的 1.85-4.36%。水飞蓟连作改善了土壤结构,促进了盐分淋溶,是土壤降盐的主要机制。结果表明,在干旱地区滴灌条件下连作Suaeda莎莎是改良盐碱地的有效方法,为干旱地区长期连作盐生植物改良盐碱地提供了理论参考。
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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.
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