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[有机物料对喀斯特土壤磷素形态及含磷细菌群落的影响]

[Effects of Organic Materials on Phosphorus Fractions and -harboring Bacterial Community in Karst Soil].

作者信息

Xia Xin, Qiao Hang, Sun Qi, Liu Kun-Ping, Chen Xiang-Bi, He Xun-Yang, Hu Ya-Jun, Su Yi-Rong

机构信息

Key Laboratory of Agro-ecological Processes in Subtropical Region, Institute of Subtropical Agriculture, Chinese Academy of Sciences, Changsha 410125, China.

University of Chinese Academy of Sciences, Beijing 100049, China.

出版信息

Huan Jing Ke Xue. 2022 Sep 8;43(9):4636-4646. doi: 10.13227/j.hjkx.202111304.

Abstract

Efficient utilization of organic materials based on the rich resources in the karst region can promote soil fertility. Microorganisms have a crucial influence on soil phosphorus availability. is considered to be the encoding phosphatase gene that can reflect the hydrolysis of organophosphorus compounds for the soil bacterial community. Molecular analysis of the -harboring bacterial gene provides insight into promoting soil phosphorus availability under different fertilization managements. However, the effects of organic materials on soil phosphorus fractions associated with -harboring bacterial communities are poorly understood. This study comprehensively investigated the effects of organic materials on soil phosphorus availability and explored environmental drivers of -harboring bacteria in the Karst region. Here, six treatments were designed in the field as follows:non-fertilized control (CK), inorganic fertilization (NPK), inorganic fertilization combined with straw (NPKS), inorganic fertilization combined with manure (NPKM), inorganic fertilization combined with sludge (NPKL), and inorganic fertilization combined with sugarcane ash (NPKA). The -harboring bacterial community in Karst region soil was analyzed using high-throughput sequencing. The results showed that the content of total P (TP), Olsen-P, and Ca-P increased with the years after organic material application, whereas the content of CaCl-P first decreased and then increased. Compared to that under the CK treatment, organic material application, especially NPKL treatment, significantly increased soil total nitrogen (TN), TP, Olsen-P, CaCl-P, and Ca-P contents, followed by those in the NPKA and NPKM treatments. Correlation analysis showed that the contents of CaCl-P, Ca-P, and Olsen-P were significantly positively correlated with soil exchangeable calcium (Ca-ex) content. Redundancy analysis (RDA) showed that TN, Ca-ex, soil organic carbon (SOC), and total potassium (TK) contents were the key factors affecting soil P fractions. Using high-throughput sequencing, we found that only NPKS increased the richness of -harboring bacteria compared to that under the control treatment. No significant difference was observed in the -harboring bacterial community among all treatments. The RDA model selected the Ca-ex, TK, Olsen-P, pH, and SOC as the key environmental predictors for the -harboring bacterial community. In summary, soil phosphorus availability can be improved through the input of organic materials and inorganic fertilizer combined with manure, sludge, and ash. These additions were suitable for nutrient management and sustainable development in farmland soil in the Karst region of Guangxi.

摘要

基于喀斯特地区丰富资源对有机物料进行高效利用能够提高土壤肥力。微生物对土壤磷有效性具有关键影响。被认为是可反映土壤细菌群落中有机磷化合物水解情况的编码磷酸酶基因。对携带该基因的细菌基因进行分子分析有助于深入了解不同施肥管理下提高土壤磷有效性的情况。然而,有机物料对与携带该基因的细菌群落相关的土壤磷组分的影响却鲜为人知。本研究全面调查了有机物料对土壤磷有效性的影响,并探究了喀斯特地区携带该基因细菌的环境驱动因素。在此,田间设计了六种处理,如下所示:不施肥对照(CK)、无机施肥(NPK)、无机施肥结合秸秆(NPKS)、无机施肥结合厩肥(NPKM)、无机施肥结合污泥(NPKL)以及无机施肥结合甘蔗灰(NPKA)。采用高通量测序分析喀斯特地区土壤中携带该基因的细菌群落。结果表明,总磷(TP)、 Olsen磷和钙磷含量随着有机物料施用年限的增加而升高,而氯化钙磷含量先下降后上升。与CK处理相比,施用有机物料,尤其是NPKL处理,显著提高了土壤全氮(TN)、TP、 Olsen磷、氯化钙磷和钙磷含量,其次是NPKA和NPKM处理。相关性分析表明,氯化钙磷、钙磷和 Olsen磷含量与土壤交换性钙(Ca-ex)含量显著正相关。冗余分析(RDA)表明,TN、Ca-ex、土壤有机碳(SOC)和全钾(TK)含量是影响土壤磷组分的关键因素。通过高通量测序,我们发现与对照处理相比,只有NPKS增加了携带该基因细菌的丰富度。所有处理间携带该基因的细菌群落未观察到显著差异。RDA模型选择Ca-ex、TK、 Olsen磷、pH和SOC作为携带该基因细菌群落的关键环境预测因子。总之,通过有机物料与无机肥料结合厩肥、污泥和灰分的投入可以提高土壤磷有效性。这些添加物适用于广西喀斯特地区农田土壤的养分管理和可持续发展。

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