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[施肥与种植模式对中国西北黄土高原农田土壤团聚体及碳分布的影响]

[Effects of fertilization and planting patterns on soil aggregate and carbon distribution in farmland of the Loess Plateau, Northwest China].

作者信息

Li Chun-Yue, Chang Shun, Zhong Fan-Xin, Xue Ying-Long, Miao Yu, Wang Yi, Dang Ting-Hui

机构信息

School of Geography and Tourism, Shaanxi Normal University, Xi'an 710119, China.

Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710061, China.

出版信息

Ying Yong Sheng Tai Xue Bao. 2021 Jan;32(1):191-200. doi: 10.13287/j.1001-9332.202101.027.

Abstract

Based on a long-term experiment in the Changwu Agro-ecological Experimental Station in Xianyang, Shaanxi, China, we examined the effects of fertilization and planting patterns on soil aggregate quantity, aggregate stability and total carbon and organic carbon distribution in different aggregate fractions through dry and wet sieving methods, as well as the TOC combustion method. There were ten treatments, including uncultivated (R), wheat continuous cropping (CK/W), wheat-corn rotation (L), and nitrogen fertilizer (N), phosphorus fertilizer (P), nitrogen and phosphorus fertilizer (NP), organic fertilizer (M), nitrogen and organic fertilizer (NM), phosphorus and organic fertilizer (PM), nitrogen and phosphorus and organic fertilizer (NPM) for CK/W. The results showed that fertilizer application and planting patterns affected soil aggregate distribution and stability, the contents and contribution rates of total C and organic C. Force-stable aggregate was mainly constituted by >0.25 mm aggregate (>67%), which was reduced by fertilization. Continuous cropping decreased micro-aggregate while rotation facilitated it and the effect was larger than fertilization. Water-stable aggregate was mainly comprised of micro-aggregate (<0.25 mm), the contribution of which was larger than 61%. Both fertilizer application and planting pattern reduced water-stable micro-aggregate. Fertilizer application and planting pattern decreased the percentage of aggregate destruction rate (PAD) and increased macro-aggregate (>0.25 mm, R) content. Organic fertilizer significantly improved total C and organic C concentrations in all the fractions of force-stable aggregates. Continuous cropping and rotation cropping increased total C concentration in all the aggregate fractions while rotation cropping significantly decreased organic C concentration. Single N and P fertilization decreased soil total C concentration, while mixed application of N and P fertilizers, and organic fertilizer significantly increased soil total C concentration. The effect of planting patterns on soil total C was lower than that of fertilization. Both continuous cropping and rotation cropping increased soil total C. Mixed application of N and P fertilizers, and organic fertilizer signifi-cantly increased soil organic C concentration while single N and P fertilization decreased it. The effect of planting patterns on soil organic C was lower than that of fertilization, while rotation cropping did not facilitate soil organic C. Micro-aggregate was the most notable size fraction to total carbon and organic C, with the contribution being 21.2%-33.6%. Fertilization and planting pattern increased the contribution rate of micro-aggregate in soil total C. NP and NPM significantly increased the contribution rate of micro-aggregate in soil total C and soil organic C. The effect of rotation cropping was most obvious in driving the contribution rate of micro-aggregate in soil total C and soil organic C.

摘要

基于在中国陕西咸阳长武农业生态试验站开展的一项长期试验,我们通过干筛法、湿筛法以及总有机碳(TOC)燃烧法,研究了施肥和种植模式对土壤团聚体数量、团聚体稳定性以及不同团聚体组分中总碳和有机碳分布的影响。试验设置了10个处理,包括撂荒地(R)、小麦连作(CK/W)、小麦-玉米轮作(L),以及针对CK/W的氮肥(N)、磷肥(P)、氮磷肥(NP)、有机肥(M)、氮有机肥(NM)、磷有机肥(PM)、氮磷有机肥(NPM)。结果表明,施肥和种植模式影响土壤团聚体分布与稳定性、总碳和有机碳含量及贡献率。力稳性团聚体主要由>0.25 mm团聚体构成(>67%),施肥会使其减少。连作会降低微团聚体数量,而轮作则促进微团聚体数量增加,且该效应大于施肥。水稳性团聚体主要由微团聚体(<0.25 mm)组成,其贡献率大于61%。施肥和种植模式均会降低水稳性微团聚体数量。施肥和种植模式降低了团聚体破坏率(PAD)百分比,增加了大团聚体(>0.25 mm,R)含量。有机肥显著提高了力稳性团聚体各组分中的总碳和有机碳浓度。连作和轮作增加了所有团聚体组分中的总碳浓度,而轮作显著降低了有机碳浓度。单施氮肥和磷肥降低了土壤总碳浓度,而氮磷肥与有机肥配施显著增加了土壤总碳浓度。种植模式对土壤总碳的影响低于施肥。连作和轮作均增加了土壤总碳。氮磷肥与有机肥配施显著增加了土壤有机碳浓度,而单施氮肥和磷肥则降低了土壤有机碳浓度。种植模式对土壤有机碳的影响低于施肥,而轮作并未促进土壤有机碳增加。微团聚体是对总碳和有机碳贡献最显著的粒径组分,贡献率为21.2%-33.6%。施肥和种植模式提高了微团聚体在土壤总碳中的贡献率。NP和NPM显著提高了微团聚体在土壤总碳和土壤有机碳中的贡献率。轮作在驱动微团聚体对土壤总碳和土壤有机碳贡献率方面的效应最为明显。

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