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Increased Corn Rotation Frequency Cropping System Impacts on Soil Functional Properties

机译:玉米轮作频率提高的耕作系统对土壤功能特性的影响

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摘要

Corn (Zea mays L.) intense rotations have become more common in the southern region of the U.S Corn Belt due to high grain production levels and economic benefits (Zhang & MacKenzie, 1997). As a result of increasing corn demand and economic competitiveness to soybean (Glycine max), many producers are altering management practices and implementing crop rotations which include more corn. This increase in corn adoption has raised concerns about the long-term sustainability of corn-intense cropping systems, and their overall impact to soil function. The objective of this study was to determine the influence of crop rotations with varying frequencies of corn and soybean on soil function in a long term (nine year) no-till management system. Soil samples were collected in the spring of 2014, at 0 to 5cm (Layer 1) and 5 to 15cm (Layer 2) depths. Soil function was represented by measurements of physical, chemical, and biological soil properties. Indicators were analyzed for previous crop effects and by calculating corn rotation frequency (CRF) ratings which were assigned to each treatment based on the total number of corn (C) years within a completed 6 year rotation cycle (e.g. S-S = 0.0, S-S-C = 0.33, C-S = 0.50, C-S-C = 0.66, C-C = 1.0). By calculating frequency, long term impacts of increased corn within rotations could be more easily identified. Plots previously in soybean averaged 33% greater water stable aggregates (WSA) in Layer 1 and 40% greater in Layer 2 compared to those previously in corn. In addition, greater electrical conductivity (EC1:1) levels were observed at 0 to 5cm when soybeans were planted previously (0 to 5cm). Surface residues, potassium (K), and magnesium (Mg) concentrations were all larger following corn. As CRF increased, favorable trends in a majority of the soil properties examined at the surface layer were observed. Soil organic carbon (SOC), water filled pore space (WFPS), soil organic matter (SOM), active carbon (AC), beta-glucosidase (beta-g), and phospholipid fatty acids (PLFA) (estimation of microbial biomass and diversity) displayed increasing trends with greater corn frequency while bulk density (BD) and EC1:1 values decreased. In addition, continuous corn had the highest concentrations of soil total nitrogen (TN). Unfavorable effects with increasing CRF included reduced soil extractable phosphorus (P) at both depths. No significant differences were observed in pHw, cation exchange capacity (CEC), calcium (Ca), or Mg based on CRF at either sampled depth. Greater CRF indicated the potential for better soil functional capacity in Layer 1, while Layer 2 showed similar functional potential among all rotation treatments.
机译:由于高谷物生产水平和经济利益,玉米(Zea mays L.)的强烈轮作在美国玉米带的南部地区变得更加普遍(Zhang&MacKenzie,1997)。由于玉米需求增加以及对大豆的经济竞争力,许多生产者正在改变管理方式并实施轮作,其中包括更多的玉米。玉米收成的增加引起了人们对玉米密集型种植系统的长期可持续性及其对土壤功能的总体影响的担忧。这项研究的目的是确定长期(九年)免耕管理系统中玉米和大豆不同频率的轮作对土壤功能的影响。在2014年春季,在0至5厘米(第1层)和5至15厘米(第2层)深度采集土壤样品。土壤功能通过物理,化学和生物土壤特性的测量来表示。分析指标对先前作物的影响,并通过计算玉米轮换频率(CRF)等级,这些等级是根据完整的6年轮换周期内的玉米(C)年总数分配给每种处理的(例如,SS = 0.0,SSC = 0.33) ,CS = 0.50,CSC = 0.66,CC = 1.0)。通过计算频率,可以更容易地识别出玉米在轮作中的长期影响。与先前的玉米相比,先前在大豆中的图平均在第1层中的水稳性骨料(WSA)高出33%,在第2层中的水稳性骨料平均高40%。此外,在以前种植大豆(0至5厘米)时,在0至5厘米处观察到更高的电导率(EC1:1)。玉米之后,表面残留,钾(K)和镁(Mg)的浓度都较大。随着CRF的增加,在表层检查到的大多数土壤特性都出现了良好的趋势。土壤有机碳(SOC),充水孔隙空间(WFPS),土壤有机质(SOM),活性炭(AC),β-葡萄糖苷酶(beta-g)和磷脂脂肪酸(PLFA)(微生物生物量和玉米频率越高,显示出增加趋势,而堆积密度(BD)和EC1:1值却下降。此外,连续玉米的土壤总氮(TN)浓度最高。 CRF增加的不利影响包括两个深度的土壤可提取磷(P)减少。在任何一个采样深度处,基于CRF的pHw,阳离子交换容量(CEC),钙(Ca)或Mg均未观察到显着差异。 CRF值越高,表明在第1层土壤中的潜在功能性越好,而第2层在所有轮作处理中均具有相似的功能性潜力。

著录项

  • 作者

    Matson, Jeremy Tyler.;

  • 作者单位

    University of Missouri - Columbia.;

  • 授予单位 University of Missouri - Columbia.;
  • 学科 Soil sciences.;Plant sciences.;Agronomy.
  • 学位 M.S.
  • 年度 2015
  • 页码 139 p.
  • 总页数 139
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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