粪肥和耕作对玉米-大豆-饲草系统粉壤土土壤碳和土壤有机质的影响

Kathleen M. Bridges, Srabani Das, Heather Neikirk, Rattan Lal
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引用次数: 0

摘要

引言俄亥俄州东北部越来越多的农场采用减少或保护性耕作方式进行管理,而采用传统或集约耕作方式的农场正在减少。此外,在种植者中使用现场农家肥是很常见的。因此,了解这些农场的各种管理做法如何影响土壤健康、土壤碳储量和作物产量是很重要的。材料和方法这项农场研究在美国中西部的温带气候下,在粉砂质壤土上进行。它侧重于耕作(犁板犁[MP]、垂直/凿耕[VT]和免耕[NT])和肥料(包括或不包括粪肥)管理做法对土壤性质的影响。本项目选择了坎菲尔德粉壤土上的12个农田和两个林地进行评估,以供参考。玉米(Zea mays L.)-大豆(Glycine max L.)轮作和混合饲料干草田是考虑的作物。在0–15和15–30两个深度评估了每个农场的作物产量以及土壤有机质(SOM)、总碳(TC)、总氮(TN)、容重、pH、土壤试验磷(P)、钾(K)和硫(S) 前2年(2020年和2021年)的研究结果如下。结果在表层土壤深度(0–15 cm),TC含量在不同耕地之间没有差异(36Mg  ha−1),但明显低于Hayfields,后者的TC含量与木材场地相同(58 Mg ha−1)。耕作对土壤P、K、S的影响不显著。方差分析显示,由于肥料的原因,没有统计学差异。在土壤表面深度,主成分分析在相似性分析(ANOSIM)的支持下确定,与耕地相比,干草田的TC、TN和SOM测量结果存在差异(R-统计 = 0.33;p = 0.001),但当15-30 cm土壤深度(R统计 = 0.17;p = 0.001)。ANOSIM还确定了一个稍微显著的(R统计量 = 0.065;p = 0.031)的差异。相关分析表明SOM与玉米产量呈正相关(r = 0.59)和TN与玉米产量(r = 0.39)。结论随着耕作强度的增加,TC没有显著损失,这可能是由于在耕地中加入了粪肥,尽管使用粪肥和不使用粪肥的田地之间只有轻微的统计差异。就大多数农场的土壤测试P而言,粪肥的使用并不有害,但应该明智地使用。将干草等多年生作物与作物生产轮作可以提高TC和TN含量。最后,增加SOM可能会增加玉米产量,但尚未确定因果关系。
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Influence of manure and tillage on soil carbon and soil organic matter in silt loam soils of corn–soybean–forage systems

Introduction

An increasing number of farms in Northeast Ohio are being managed under reduced or conservation tillage practices, while those under conventional or intensive tillage are decreasing. Additionally, the use of on-site farm manure among the growers is commonplace. Therefore, it is important to understand how the various management practices of these farms are impacting soil health, soil carbon stocks and crop yields.

Materials and Methods

This on-farm study takes place in the temperate climate of the midwestern United States on a silt loam soil. It focuses on the impact of tillage (mouldboard plough [MP], vertical/chisel tillage [VT] and no-tillage [NT]) and fertilizer (manure included or not) management practices on soil properties. Twelve agriculture fields and two woodland sites, for reference, on Canfield silt loam soils were selected for assessment in this project. Corn (Zea mays L.)–soybean (Glycine max L.) rotations and mixed forage Hayfields were the crops considered. Crop yields at each farm along with soil organic matter (SOM), total carbon (TC), total nitrogen (TN), bulk density, pH, soil test phosphorus (P), potassium (K) and sulphur (S) were assessed at two depths, 0–15 and 15–30 cm. Results of the first 2 years of the study (2020 and 2021) are presented here.

Results

At the surface soil depth (0–15 cm), TC content was not different among cultivated fields (36 Mg  ha−1), but was significantly less than Hayfields, which had the same amount of TC as the wood sites (58 Mg ha−1). There was no significant difference in soil test P, K or S due to tillage. Analysis of variance revealed no statistical difference due to fertilizer. At the soil surface depth, principal component analysis, supported by analysis of similarities (ANOSIM), determined that measurements of TC, TN and SOM distinguished a difference in Hayfields compared to cultivated fields (R-statistic = 0.33; p = 0.001), but little difference when the 15–30 cm soil depth was considered (R-statistic = 0.17; p = 0.001). ANOSIM also determined a slightly significant (R-statistic = 0.065; p = 0.031) difference in fertilizer at the deeper soil depth. Correlation analysis revealed a strong positive relationship between SOM and corn grain yield (r = 0.59) and TN and corn grain yield (r = 0.39).

Conclusions

There was no significant loss of TC among increasing tillage intensities possibly due to the inclusion of manure fertilizer in tilled fields even though there were only slight statistical differences between fields that utilized manure and those that did not. The use of manure was not detrimental in terms of soil test P for most farms, but should be used judiciously. Inclusion of perennial crops such as hay in rotation with crop production can improve TC and TN content. Finally, increasing SOM could potentially increase corn grain yield, but no causal relationship has been determined yet.

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