Insights on soil carbon cycling in intercropped maize-forage systems as affected by nitrogen

IF 5.6 1区 农林科学 Q1 SOIL SCIENCE
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Abstract

Intercropping maize with forage grasses is an economical and environmentally sound practice that is increasingly being adopted to enhance resilience in tropical agriculture. Although intensifying integrated cropping systems can increase the sequestration of carbon (C) from plant residues, it also unleashes priming of old soil C enhancing C cycling, particularly under nitrogen (N) fertilization. However, the extent of these competing processes in intercropped maize–forage systems is poorly understood. This four-year study assessed whether new C inputs from maize (Zea mays) intercropped with ruzigrass (Urochloa ruziziensis), palisade grass (Urochloa brizantha), or Guinea grass (Megathyrsus maximum) in the presence or absence of N fertilization affect soil aggregation and C cycling in the soil and within macroaggregates (>0.250 mm) and microaggregates (<0.250 mm) down the soil profile. C cycling was assessed by measuring variations in the abundance of the natural isotope 13C. N fertilization of the intercropped maize–forage systems reduced the proportion of aggregates > 2 mm and the mean weight diameter of aggregates by reducing soil pH. Under N fertilization, the geometric mean diameter of aggregates were 42 % larger under palisade than under Guinea grass. New C inputs from intercropping maize with forage grasses promoted C cycling in bulk soil, particulate organic matter (POM), mineral-associated organic matter (MAOM), and macro- and microaggregates, although these effects were restricted to topsoil. No N fertilization increased ruzigrass C input into MAOM with no clear link with 13C enrichment, suggesting that N fertilization does not impair C stabilization in this pool. Aggregates >2 mm and >0.5 mm were key sinks of C and N up to a soil depth of 40 cm in this intercropped system. Our findings provide insights into the extension of C cycling across SOM pools and aggregates, and the role of N management in intercropping maize forage systems.

Abstract Image

玉米-秸秆间作系统土壤碳循环受氮影响的启示
玉米与牧草间作是一种既经济又环保的做法,越来越多的人采用这种做法来提高热带农业的恢复能力。虽然强化综合耕作系统可以增加植物残留物的碳固存,但它也会释放土壤中的旧碳,促进碳循环,尤其是在施氮肥的情况下。然而,人们对玉米-秸秆间作系统中这些竞争过程的程度还知之甚少。这项为期四年的研究评估了在施氮肥或不施氮肥的情况下,玉米()与鲁茨草()、宫粉草()或几内亚草()间作所产生的新碳输入是否会通过降低土壤 pH 值而影响土壤聚集以及土壤中和大聚集体(>0.250 毫米)和微聚集体(2 毫米和聚集体平均重量直径)内的碳循环。在施氮肥的情况下,宫粉禾的聚集体几何平均直径比几内亚禾大 42%。玉米与牧草间作所产生的新碳输入促进了大体积土壤、微粒有机物、矿质相关有机物以及宏观和微观团聚体中的碳循环,但这些影响仅限于表层土壤。不施用氮肥会增加芦竹草对 MAOM 的碳输入,但与碳富集并无明显联系,这表明施用氮肥不会影响该池中碳的稳定。在这个间作系统中,大于 2 毫米和大于 0.5 毫米的团聚体是碳和氮的主要吸收汇,其吸收深度可达 40 厘米。我们的研究结果有助于深入了解碳循环在 SOM 池和聚集体之间的延伸,以及氮管理在间作玉米饲草系统中的作用。
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来源期刊
Geoderma
Geoderma 农林科学-土壤科学
CiteScore
11.80
自引率
6.60%
发文量
597
审稿时长
58 days
期刊介绍: Geoderma - the global journal of soil science - welcomes authors, readers and soil research from all parts of the world, encourages worldwide soil studies, and embraces all aspects of soil science and its associated pedagogy. The journal particularly welcomes interdisciplinary work focusing on dynamic soil processes and functions across space and time.
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