Spatially refined salinity hazard analysis in gypsum-affected irrigated soils

IF 1.3 Q3 AGRONOMY Agrosystems, Geosciences & Environment Pub Date : 2024-07-04 DOI:10.1002/agg2.20539
Ansley J. Brown, Allan A. Andales, Timothy K. Gates
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Abstract

The global extent of salt-affected agricultural land, 20% of which is deemed gypsiferous, results in billions of dollars of annual economic loss, a serious problem deserving of attention. However, the analysis of gypsiferous saline soils, such as in the irrigated Lower Arkansas River Valley (LARV) of Colorado, can result in an inflated estimation of soil salinity when using the traditional soil saturated paste extract electrical conductivity (ECe), leading to inaccurate crop yield loss predictions and misguided decisions for remediation. Sparingly soluble gypsum (CaSO4 · $\cdot$ 2H2O) in these soils dissolves more readily during laboratory preparation of saturated paste extracts because of excess soil water dilution coupled with sample disturbance. We present a pragmatic linear-regression approach to correct for this phenomenon, calibrated using two adapted methods for correcting ECe on an individual sample basis. The novel approach used electrical conductivity of pore water samples from saline fields to evaluate the accuracy of the correction methods. The approach was applied on soil samples from two surface-irrigated, saline fields in the LARV, which were mapped using electromagnetic induction data and analysis of covariance linear regression, calibrated for ECe and ECe corrected for excess gypsum dissoultion (ECeg). Average ECeg values are as much as 26% lower than uncorrected ECe in gypsum-biased portions of the fields. Estimation of corn salinity hazard in these gypsum-affected areas using ECeg in lieu of ECe in a traditional yield response function generated mean relative yield values that are higher by up to 13 percentage points. We discuss lessons learned and suggest enhancements to the techniques.

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受石膏影响的灌溉土壤的空间精细盐度危害分析
全球受盐分影响的农田面积达 20%,其中 20% 被认为是石膏盐碱地,每年造成数十亿美元的经济损失,这一严重问题值得关注。然而,在对科罗拉多州阿肯色河下游河谷(LARV)等灌溉区的石膏盐碱土进行分析时,如果使用传统的土壤饱和糊状提取物电导率(ECe),可能会导致对土壤盐分的估算偏高,从而导致对作物产量损失的预测不准确,并做出错误的修复决策。在实验室制备饱和糊状提取物的过程中,这些土壤中的稀溶性石膏(CaSO4 - $\cdot$ 2H2O)更容易溶解,这是因为过量的土壤水稀释加上样品扰动造成的。我们提出了一种实用的线性回归方法来校正这一现象,并使用两种经过调整的方法来校正单个样品的导电率。新方法使用盐田孔隙水样本的电导率来评估校正方法的准确性。该方法应用于 LARV 地区两块地表灌溉盐碱地的土壤样本,利用电磁感应数据和协方差线性回归分析绘制了盐碱地地图,校正了导电率(ECe)和经石膏过量溶解(ECeg)校正的导电率(ECe)。在有石膏偏向的田块中,ECeg 平均值比未经校正的 ECe 低 26%。在这些受石膏影响的地区,用 ECeg 代替传统产量反应函数中的 ECe 来估算玉米盐渍化危害,得出的平均相对产量值高达 13 个百分点。我们讨论了经验教训,并提出了改进技术的建议。
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来源期刊
Agrosystems, Geosciences & Environment
Agrosystems, Geosciences & Environment Agricultural and Biological Sciences-Agricultural and Biological Sciences (miscellaneous)
CiteScore
2.60
自引率
0.00%
发文量
80
审稿时长
24 weeks
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