Analyzing the Impact of Storm ‘Daniel’ and Subsequent Flooding on Thessaly’s Soil Chemistry through Causal Inference

M. Iatrou, M. Tziouvalekas, Alexandros Tsitouras, Elefterios Evangelou, C. Noulas, D. Vlachostergios, V. Aschonitis, Georgios Arampatzis, Irene Metaxa, Christos Karydas, P. Tziachris
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Abstract

Storm ‘Daniel’ caused the most severe flood phenomenon that Greece has ever experienced, with thousands of hectares of farmland submerged for days. This led to sediment deposition in the inundated areas, which significantly altered the chemical properties of the soil, as revealed by extensive soil sampling and laboratory analysis. The causal relationships between the soil chemical properties and sediment deposition were extracted using the DirectLiNGAM algorithm. The results of the causality analysis showed that the sediment deposition affected the CaCO3 concentration in the soil. Also, causal relationships were identified between CaCO3 and the available phosphorus (P-Olsen), as well as those between the sediment deposit depth and available manganese. The quantified relationships between the soil variables were then used to generate data using a Multiple Linear Perceptron (MLP) regressor for various levels of deposit depth (0, 5, 10, 15, 20, 25, and 30 cm). Then, linear regression equations were fitted across the different levels of deposit depth to determine the effect of the deposit depth on CaCO3, P, and Mn. The results revealed quadratic equations for CaCO3, P, and Mn as follows: 0.001XCaCO32 + 0.08XCaCO3 + 6.42, 0.004XP2 − 0.26XP + 12.29, and 0.003XMn2 − 0.08XMn + 22.47, respectively. The statistical analysis indicated that corn growing in soils with a sediment over 10 cm requires a 31.8% increase in the P rate to prevent yield decline. Additional notifications regarding cropping strategies in the near future are also discussed.
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通过因果推论分析 "丹尼尔 "风暴及随后的洪水对塞萨利土壤化学的影响
丹尼尔 "风暴造成了希腊有史以来最严重的洪水现象,数千顷农田被淹没多日。大量的土壤取样和实验室分析表明,洪水导致沉积物在淹没区沉积,极大地改变了土壤的化学性质。使用 DirectLiNGAM 算法提取了土壤化学性质与沉积物沉积之间的因果关系。因果关系分析结果表明,沉积物沉积影响了土壤中 CaCO3 的浓度。此外,还确定了 CaCO3 与可用磷(P-Olsen)之间的因果关系,以及沉积深度与可用锰之间的因果关系。然后,使用多重线性感知器(MLP)回归器生成不同沉积深度(0、5、10、15、20、25 和 30 厘米)的土壤变量之间的量化关系数据。然后,拟合不同沉积深度的线性回归方程,以确定沉积深度对 CaCO3、P 和 Mn 的影响。结果显示 CaCO3、P 和 Mn 的二次方程如下:分别为 0.001XCaCO32 + 0.08XCaCO3 + 6.42、0.004XP2 - 0.26XP + 12.29 和 0.003XMn2 - 0.08XMn + 22.47。统计分析结果表明,在沉积物超过 10 厘米的土壤中种植玉米,需要增加 31.8%的钾,才能防止产量下降。此外,还讨论了有关近期种植策略的其他通知。
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