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作物类型转变对典型黄河灌区土壤磷形态及微生物功能多样性的影响

Effect of Crop Type Shift on Soil Phosphorus Morphology and Microbial Functional Diversity in a Typical Yellow River Irrigation Area.

作者信息

Xie Zijian, Zhao Rongbo, Bo Bo, Li Chunhua, Wang Yang, Chu Yu, Ye Chun

机构信息

National Engineering Laboratory for Lake Pollution Control and Ecological Restoration, Chinese Research Academy of Environmental Sciences, Beijing 100012, China.

Key Laboratory of Drinking Water Source Protection of the Ministry of Ecology and Environment, Chinese Research Academy of Environmental Sciences, Beijing 100012, China.

出版信息

Microorganisms. 2025 Jun 23;13(7):1458. doi: 10.3390/microorganisms13071458.

Abstract

The Hetao irrigation area is one of the largest irrigation areas in the Yellow River Basin and a typical salinized agricultural area. Crop type shifts in this area can alter soil phosphorus (P) morphology and microbial functional diversity, thereby influencing soil P losses. However, few studies have elucidated the underlying mechanisms. In this study, soil samples were collected from four different crop planting areas: sunflower field (SF), corn field (CF), wheat land (WL), and vegetable and fruit land (VFL). Subsequently, the physicochemical properties, P fractions, and phosphate-solubilizing microorganisms (PSMs) were analyzed. The results indicated that when other lands shifted to SF, the soil pH increased significantly. Simultaneously, SOM, TN, and TP decreased significantly during the crop type conversion. Analysis of P fraction revealed that moderately active P, including NaOH-P, NaOH-P, and HCl-P, were the dominant fractions in the tested soils. Among them, HCl-P was the major component of moderately active P. The soil P leaching change point in the tested are was 6.25 mg Olsen-P kg. The probabilities of P leaching in WL, VFL, CF, and SF were 91.7%, 83.8%, 83.8%, and 66.7%, respectively. Additionally, the sum of the relative abundances of the three PSMs in SF, VFL, WL, and CF were 8.81%, 11.88%, 8.03%, and 10.29%, respectively. The shift in crop type to SF exacerbated the soil degradation process. Both TP and residual P in the soil decreased. However, the NaHCO slightly increased, which may have been due to the increased abundance of and .

摘要

河套灌区是黄河流域最大的灌区之一,也是典型的盐碱化农业区。该地区作物类型的转变会改变土壤磷(P)形态和微生物功能多样性,从而影响土壤磷流失。然而,很少有研究阐明其潜在机制。本研究从四个不同的作物种植区采集土壤样本:向日葵田(SF)、玉米田(CF)、小麦地(WL)和蔬菜水果地(VFL)。随后,分析了土壤的理化性质、磷组分和溶磷微生物(PSM)。结果表明,当其他土地转变为向日葵田时,土壤pH值显著升高。同时,在作物类型转换过程中,土壤有机碳(SOM)、全氮(TN)和全磷(TP)显著下降。磷组分分析表明,包括NaOH-P、NaOH-P和HCl-P在内的中等活性磷是测试土壤中的主要组分。其中,HCl-P是中等活性磷的主要成分。测试区域土壤磷淋溶变化点为6.25 mg Olsen-P/kg。WL、VFL、CF和SF中磷淋溶的概率分别为91.7%、83.8%、83.8%和66.7%。此外,SF、VFL、WL和CF中三种PSM相对丰度之和分别为8.81%、11.88%、8.03%和10.29%。作物类型向向日葵田的转变加剧了土壤退化过程。土壤中的TP和残留磷均下降。然而,NaHCO略有增加,这可能是由于[此处原文缺失部分内容]丰度增加所致。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/a99f/12299866/78d6336b9303/microorganisms-13-01458-g001.jpg

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