首页> 外文期刊>Geoderma: An International Journal of Soil Science >Long-term manure and fertilizer effects on soil organic matter fractions and microbes under a wheat-maize cropping system in northern China
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Long-term manure and fertilizer effects on soil organic matter fractions and microbes under a wheat-maize cropping system in northern China

机译:北方小麦-玉米种植体系下长期肥料和肥料对土壤有机质和微生物的影响

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As an essential indicator of soil quality, soil organic carbon (SOC) and its different labile fractions have an important role in determining soil chemical, physical, and biological properties. The objective of this study was to evaluate the soil carbon (C) and nitrogen (N) contents in different soil organic matter (SOM) pools (light and heavy fractions), the role of light- and heavy-fraction C in SOC sequestration, and culturable microbial counts in the surface (0-20 cm) of a fluvo-aquic soil after 18 years of fertilization treatments under a wheat-maize cropping system in the North China Plain. The experiment included seven treatments: (1) OM, organic manure; (2) 1/2OMN, half organic manure with mineral fertilizer NPK; (3) NPK, mineral fertilizer NPK; (4) NP, mineral fertilizer NP; (5) PK, mineral fertilizer PK; (6) NK, mineral fertilizer NK; and (7) CK, unfertilized control. Carbon and N contents of the light and heavy fractions were highest in the CM treatment, while the CK treatment showed the lowest value. Application of half organic manure with mineral fertilizer NPK (treatment 2) significantly increased C and N contents of the light and heavy fractions in soil in comparison with application of mineral fertilizer alone (treatments 3, 4, 5, and 6). For the mineral fertilizer treatments, a balanced application of NPK (treatment 3) showed higher C and N contents of the light and heavy fractions than an unbalanced use of fertilizers (treatments 4, 5, and 6). Heavy-fraction C dominated total SOC storage in all treatments. The total SOC increase under fertilization treatments is attributed to an increase in C content of both the light and the heavy fraction. However, the SOC increase for the manure treatments was mainly due to an increase in the C content of the heavy fraction, whereas that for mineral fertilizer treatments was mainly due to an increase in the C content of the light fraction. The total soil culturable microbial counts (including bacteria, fungi, and actinomycetes) was observed to be highest for the OM treatment, while the control plot showed the lowest value. Application of half organic manure with mineral fertilizer NPK was found to produce a higher culturable microbial counts than application of mineral fertilizers alone, and the NPK treatment gave a higher culturable microbial counts than other mineral fertilizer treatments (NP, PK or NK). Light-fraction C is probably the better predictor of microbial abundance, as it correlated more strongly with culturable microbial counts than total SOC did. Crown Copyright (C) 2008 Published by Elsevier B.V. All rights reserved.
机译:作为土壤质量的重要指标,土壤有机碳(SOC)及其不同的不稳定组分在决定土壤化学,物理和生物学特性方面具有重要作用。这项研究的目的是评估不同土壤有机质(SOM)池(轻组分和重组分)中土壤碳(C)和氮(N)的含量,轻组分和重组分C在SOC螯合中的作用,在华北平原小麦-玉米种植系统中,经过18年的施肥处理后,潮潮土壤表面(0-20厘米)的可培养微生物数量。实验包括七种处理方法:(1)OM,有机肥料; (2)1 / 2OMN,半有机肥料和矿物肥料NPK; (3)氮磷钾,矿物肥料氮磷钾; (4)NP,矿物肥料NP; (5)PK,矿物肥料PK; (6)NK,矿物肥料NK; (7)CK,未受精对照。轻,重馏分的碳和氮含量在CM处理中最高,而CK处理显示最低。与单独施用矿物肥料(处理3、4、5和6)相比,施用半有机肥料和矿物肥料NPK(处理2)可显着增加土壤中轻重组分的碳和氮含量。对于矿物肥料处理,氮磷钾的平衡施用(处理3)比轻度不平衡的肥料(处理4、5和6)显示出较高的轻,重组分碳和氮含量。在所有处理中,重馏分C占总SOC储存量。施肥处理下总SOC的增加归因于轻组分和重组分中C含量的增加。但是,粪肥处理的SOC增加主要是由于重组分中C含量的增加,而矿物肥料处理的SOC主要是由于轻质组分中C含量的增加。 OM处理的土壤可培养微生物总数(包括细菌,真菌和放线菌)最高,而对照图显示最低。发现使用半有机肥和矿物肥料NPK比单独施用矿物肥料产生的可培养微生物数量更高,并且NPK处理比其他矿物肥料处理(NP,PK或NK)产生的可培养微生物数量更高。轻馏分C可能是微生物丰度的更好预测指标,因为与总SOC相比,轻馏分C与可培养微生物数的相关性更高。 Crown版权所有(C)2008,Elsevier B.V.保留所有权利。

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