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Watershed-scale soil quality assessment: Assessing reasons for poor canopy development in corn

机译:流域规模的土壤质量评估:评估玉米天覆开发差的原因

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Soil quality assessment is a critical component in understanding the long-term effects of soil and crop management practices within agricultural watersheds. Additionally, simple, robust assessment methodologies are needed for policy planning and implementation. In the South Fork of the Iowa River Watershed, an aerial survey was conducted during the summer of 2006, and fields that were planted to corn and appeared to have sections with underdeveloped canopy were marked. Our objective was to determineif a soil quality assessment could suggest the reasons for the poor canopy development. Fifty-one marked fields were assessed in autumn of 2006. Four composite samples were taken at the 0-10 cm depth in each field, three from the dominant soil types in the field and the fourth from the area with poor canopy. Bulk density (BD), aggregate stability, texture, pH, extractable P, K, Ca, Mg, N03, Cu, Fe, Mn and Zn, electrical conductivity (EC), soil organic carbon (SOC), total N, microbial biomass C (MBC), potentially mineralizable C (C^and N (N^), and (3-glucosidase (BG) activity were measured. The Soil Management Assessment Framework (SMAF) was used to assess soil quality. There was no single cause for poor canopy across in all fields. Overall, the SOC, MBC, Cmin, Nmin, and BG activity were lower in the areas with poor canopy development. SMAF indicator scores for carbon, which compensate for differing soil types, were significantly lower for the poor canopy areas. When the data means were analysed, SOC,MBC, BD and EC, as well as the soil quality index (SQI, mean of the 11 scored indicators) were significantly different between the normal and poor canopy areas. On a field to field basis, there were specific problems such as low SOC and other indicationsof poor nutrient cycling: low extractable P, high BD, and low water-filled pore space at time of sampling. When the fields were separated by slope position, most indicators and indicator scores were significantly lower in the poor canopy areas. Using SMAF to determine specific problems will help land managers deyelop management practices to ameliorate poor performing field areas. Policy makers can use information like this to assess overall effectiveness of management systems on ecosystem functions.
机译:土壤质量评估是了解农业流域土壤和作物管理实践的长期影响方面的关键组成部分。此外,策略规划和实施需要简单,鲁棒的评估方法。在爱荷华河流域的南叉,在2006年夏天进行了一项空中调查,并在玉米种植并似乎具有欠发达的树冠的田间的田地进行了标记。我们的目标是确定,如果土壤质量评估可能暗示冠层开发差的原因。 2006年秋季评估了五十一张标记的田地。在每个场的0-10厘米的深度下进行了四种复合样品,其中三种来自该领域的主要土壤类型,其中三个来自覆盆子差的区域。堆积密度(BD),骨料稳定性,质地,pH,可提取的P,K,Ca,Mg,N03,Cu,Fe,Mn和Zn,导电性(EC),土壤有机碳(SoC),总N,微生物生物量C(MBC),潜在的可融集C(C 1和N(N ^)和(3-葡糖苷酶(BG)活性。土壤管理评估框架(SMAF)用于评估土壤质量。没有单一原因对于所有领域的贫困天覆。总体而言,冠层开发差的区域,SOC,MBC,CMIN,NMIN和BG活性较低。用于弥补不同土壤类型的碳的SMAF指示剂分数显着降低差的树木区域。分析数据装置,SoC,MBC,BD和EC,以及土壤质量指数(SQI,11分别指标的平均值)在正常和可怜的树冠区域之间显着差异。在一个领域到现场基础上,有特定的问题,如低SoC和其他指示营养循环差:低可提取物在取样时,P,高BD和低水填充孔隙空间。当通过坡度位置分离场时,差距在可差的顶篷区域中大多数指标和指标分数显着降低。使用SMAF来确定特定问题将有助于土地管理人员脱离管理实践改善糟糕的表演场地。政策制定者可以使用这样的信息来评估管理系统对生态系统功能的整体效力。

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