Evaluation of spatial variability of physico-chemical indicators of chernozem podzolic with the using of precise agriculture technologies

S. Sychevskyy, O. Tonkha, O. Pikovska
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Abstract

On the experimental fields of “Lotivka Elite” LLC of Shepetivka district of Khmelnytsky region the estimation of spatial heterogeneity of indicators of physical and chemical properties of chernozem podzolic was carried out. Statistical analysis of the data was performed on the following indicators: number of observations (n); average value (Xav); standard deviation (S); coefficient of variation (Cv); absolute error of the mean (SXav). The analysis of the probability of the nature of the humus content was performed according to the humus content index - the ratio of the actual humus content at the control point to the arithmetic mean. It is revealed that the probability of manifestation of average (typical) values of humus content at the studied object does not exceed 50%, deviations of probabilities from the average level of humus content in the direction of decrease do not exceed 40% of territorial distribution. Spatial variability of humus and mobile calcium content is average, CV is 19–23% (10 more CV less than 25). Statistical parameter of calcium content in the soil layer 0-30 cm on average - 252.4 ± 10.0, maximum - 350.0 ± 9.11 mg on 100 g of soil. In general, the field is dominated by soils with a content of mobile calcium 240.0-290.0 mg on 100 g of soil. Active acidity was characterized by low variability, the average was 6.5 ± 0.3, the maximum - 7.3 ± 0.2 pH units. The yield of winter wheat had a low degree of variability with an average of 87.4 ± 4.3 c on ha.
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应用精准农业技术评价黑钙土灰化土理化指标的空间变异性
在赫梅利尼茨基地区谢佩蒂夫卡区“Lotivka Elite”有限责任公司的试验田上,对黑钙土灰化土理化指标的空间异质性进行了估算。对数据进行以下指标的统计分析:观察次数(n);平均值(Xav);标准偏差S;变异系数;绝对均值误差(SXav)。根据腐殖质含量指数-在控制点的实际腐殖质含量与算术平均值的比率,对腐殖质含量性质的概率进行分析。结果表明,研究对象腐殖质含量平均(典型)值出现的概率不超过50%,腐殖质含量下降方向与平均水平的概率偏差不超过区域分布的40%。腐殖质和流动钙含量的空间变异性平均,CV值为19 ~ 23% (CV值大于10,CV值小于25)。0-30 cm土层中钙含量统计参数平均值为- 252.4±10.0 mg,最大值为- 350.0±9.11 mg / 100 g土壤。一般情况下,以100 g土壤中流动钙含量为240.0 ~ 290.0 mg的土壤为主。活性酸度具有较低的变异性,平均值为6.5±0.3,最大值为- 7.3±0.2 pH单位。冬小麦产量变异程度较低,平均为87.4±4.3℃/公顷。
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