
Figure 1:
Layout schematic of a 6 × 10 grid sampling of contiguous quadrats (20 m × 45 m) in the commercial red raspberry production field WA-2 located in Lynden, WA. From the center of each quadrat (red dot), above-ground disease severity was visually assessed and rated; soil and root samples were collected to quantify Phytophthora rubi, Pratylenchus penetrans, and soil texture (sand, silt, clay); and surface field elevations were also recorded at each sampling point.
Table 1:
Exploratory data analysis of disease rating, Phytophthora rubi DNA concentrations in roots, Pratylenchus penetrans densities in roots and soil, soil texture, and elevation in four commercial red raspberry production fields in Oregon (OR-1 and OR-2) and Washington (WA-1 and WA-2).
| Field | Variables | Mean | SE | Standard deviation | VIRa |
|---|---|---|---|---|---|
| OR-1 | Disease rating | 6.53 | 0.18 | 1.37 | 0.29 |
| P. rubi DNA (ng/g root) | 681.87 | 192.78 | 1,493.29 | 3,270.30 | |
| P. penetrans/g root | 16.78 | 4.80 | 37.16 | 82.29 | |
| P. penetrans/g soil | 50.38 | 10.62 | 82.25 | 134.27 | |
| % sand | 27.93 | 0.50 | 3.90 | 0.54 | |
| % silt | 51.45 | 0.45 | 3.50 | 0.24 | |
| % clay | 20.61 | 0.34 | 2.61 | 0.33 | |
| Elevation (m) | 6.43 | 0.38 | 2.92 | 1.33 | |
| OR-2 | Disease rating | 3.65 | 0.08 | 0.62 | 0.10 |
| P. rubi DNA (ng/g root) | 91.75 | 64.48 | 499.49 | 2,719.20 | |
| P. penetrans/g root | 337.32 | 79.88 | 618.74 | 1,134.95 | |
| P. penetrans/g soil | 86.05 | 9.06 | 70.17 | 57.22 | |
| % sand | 27.93 | 0.89 | 6.87 | 1.69 | |
| % silt | 45.97 | 0.88 | 6.88 | 1.03 | |
| % clay | 26.53 | 0.44 | 3.44 | 0.45 | |
| Elevation (m) | 0.66 | 0.05 | 0.39 | 0.23 | |
| WA-1 | Disease rating | 3.26 | 0.23 | 1.79 | 0.98 |
| P. rubi DNA (ng/g root) | 1,106.31 | 514.86 | 3,988.13 | 14,376.77 | |
| P. penetrans/g root | 16.16 | 5.96 | 46.19 | 132.06 | |
| P. penetrans/g soil | 26.77 | 4.89 | 37.91 | 53.67 | |
| % sand | 62.60 | 0.89 | 6.87 | 0.75 | |
| % silt | 27.27 | 0.72 | 5.57 | 1.14 | |
| % clay | 10.13 | 0.29 | 2.26 | 0.50 | |
| Elevation (m) | 1.74 | 0.13 | 1.00 | 0.58 | |
| WA-2 | Disease rating | 5.47 | 0.22 | 1.73 | 0.54 |
| P. rubi DNA (ng/g root) | 817.32 | 440.91 | 3,415.25 | 14,270.84 | |
| P. penetrans/g root | 598.35 | 97.64 | 756.33 | 956.02 | |
| P. penetrans/g soil | 178.42 | 26.01 | 201.51 | 227.58 | |
| % sand | 34.01 | 1.01 | 7.85 | 1.81 | |
| % silt | 51.75 | 0.92 | 7.11 | 0.98 | |
| % clay | 14.25 | 0.41 | 3.18 | 0.71 | |
| Elevation (m) | 1.43 | 0.09 | 0.73 | 0.37 |
Table 2:
Global Moran’s I for assessing spatial autocorrelation in disease rating, Phytophthora rubi DNA concentrations in roots, Pratylenchus penetrans densities in roots and soil, soil texture, and elevation in four commercial red raspberry production fields in Oregon (OR-1 and OR-2) and Washington (WA-1 and WA-2).
| Field | Variables | Moran’s I coefficienta | P-valueb |
|---|---|---|---|
| OR-1 | Disease rating | 0.28 | <0.001 |
| P. rubi DNA in root | 0.07 | 0.001 | |
| P. penetrans in root | 0.04 | 0.08 | |
| P. penetrans in soil | 0.04 | 0.07 | |
| Sand | 0.11 | <0.001 | |
| Silt | 0.10 | 0.002 | |
| Clay | 0.18 | <0.001 | |
| Elevation | 0.75 | <0.001 | |
| OR-2 | Disease rating | 0.01 | 0.22 |
| P. rubi DNA in root | −0.02 | 0.53 | |
| P. penetrans in root | −0.01 | 0.40 | |
| P. penetrans in soil | 0.06 | 0.01 | |
| Sand | 0.07 | 0.009 | |
| Silt | 0.06 | 0.01 | |
| Clay | 0.02 | 0.20 | |
| Elevation | 0.10 | 0.002 | |
| WA-1 | Disease rating | 0.21 | <0.001 |
| P. rubi DNA in root | 0.08 | 0.003 | |
| P. penetrans in root | 0.004 | 0.29 | |
| P. penetrans in soil | 0.31 | <0.001 | |
| Sand | 0.28 | <0.001 | |
| Silt | 0.19 | <0.001 | |
| Clay | 0.31 | <0.001 | |
| Elevation | 0.59 | <0.001 | |
| WA-2 | Disease rating | 0.51 | <0.001 |
| P. rubi DNA in root | 0.22 | <0.001 | |
| P. penetrans in root | 0.09 | 0.003 | |
| P. penetrans in soil | 0.11 | <0.001 | |
| Sand | 0.42 | <0.001 | |
| Silt | 0.22 | <0.001 | |
| Clay | 0.43 | <0.001 | |
| Elevation | 0.53 | <0.001 |
a Global Moran’s I coefficient values range from −1 to 1, where a value <0 indicates negative spatial autocorrelation and a value >0 indicates positive spatial autocorrelation. A positive spatial autocorrelation indicates the presence of clustering, i.e., nearby areas have similar attribute values, whereas a negative spatial autocorrelation indicates dissimilarities in neighborhood data attribute values.

Figure 2:
LISA for disease rating, Phytophthora rubi DNA concentrations in roots, and Pratylenchus penetrans densities in roots and soil in four commercial red raspberry production fields in Oregon (OR-1 and OR-2) and Washington (WA-1 and WA-2). A positive value for the local Moran’s I indicates that a sampling point has a similar attribute value to the neighboring points (clusters), and a negative value indicates dissimilar attribute values in the local neighborhood (outliers). Solid-filled black shapes indicate the significance of the local Moran’s I coefficient at P < 0.05. LISA, local indicators of spatial association.

Figure 3:
Moran scatterplot for disease rating, Phytophthora rubi DNA concentrations in roots, and Pratylenchus penetrans densities in roots and soil in four commercial red raspberry production fields in Oregon (OR-1 and OR-2) and Washington (WA-1 and WA-2). The scatterplot is characterized by four quadrants corresponding to the four types of spatial association and illustrates relationships between an individual sampling value (standardized observation) and the average values at neighboring sampling points (standardized spatial lags). The lower left and upper right quadrants indicate spatial clustering or PSA. The lower left quadrant is characterized by low values for both the spatial lags and the observations (Low–Low), and in the upper right quadrant, there are high values for both the spatial lags and the observations (High–High). The upper left (Low–High) and lower right (High–Low) quadrants indicate spatial outliers or NSA. The slope of each regression line corresponds to the Moran’s I coefficients listed in Table 2. NSA, negative spatial association; PSA, positive spatial association.

Figure 4:
LISA for soil texture (sand, silt, and clay) and field elevation in four commercial red raspberry production fields in Oregon (OR-1 and OR-2) and Washington (WA-1 and WA-2). A positive value for the local Moran’s I indicates that a sampling point has a similar attribute value to the neighboring points (clusters), and a negative value indicates dissimilar attribute values in the local neighborhood (outliers). Solid-filled black shapes indicate the significance of the local Moran’s I coefficient at P < 0.05. LISA, local indicators of spatial association.

Figure 5:
Moran scatterplot for soil texture (sand, silt, and clay) and field elevation in four commercial red raspberry production fields in Oregon (OR-1 and OR-2) and Washington (WA-1 and WA-2). The scatterplot is characterized by four quadrants corresponding to the four types of spatial association and illustrates relationships between an individual sampling value (standardized observation) and the average values at neighboring sampling points (standardized spatial lags). The lower left and upper right quadrants indicate spatial clustering or PSA. The lower left quadrant is characterized by low values for both the spatial lags and the observations (Low–Low), and in the upper right quadrant, there are high values for both the spatial lags and the observations (High–High). The upper left (Low–High) and lower right (High–Low) quadrants indicate spatial outliers or NSA. The slope of each regression line corresponds to the Moran’s I coefficients listed in Table 2. NSA, negative spatial association; PSA, positive spatial association.

Figure 6:
Experimental variogram graph for assessing the spatial structure of disease rating, Phytophthora rubi DNA concentrations in roots, and Pratylenchus penetrans densities in roots and soil in four commercial red raspberry production fields in Oregon (OR-1 and OR-2) and Washington (WA-1 and WA-2). The x-axis shows the distance lag, which is created by plotting the average variability between pairs of sampling points, and the y-axis shows the calculated value of the semivariance, where a greater value indicates less spatial correlation between pairs of points. The variogram model type and fitting parameters for each commercial field are listed in Table 3.

Figure 7:
Experimental variogram graph for assessing the spatial structure of soil texture (sand, silt, and clay) and field elevation in four commercial red raspberry production fields in Oregon (OR-1 and OR-2) and Washington (WA-1 and WA-2). The x-axis shows the distance lag, which is created by plotting the average variability between pairs of sampling points, and the y-axis shows the calculated value of the semivariance, where a greater value indicates less spatial correlation between pairs of points. The variogram model type and fitting parameters for each commercial field are listed in Table 3.
Table 3:
Fitted models for the experimental variogram analysis for quantifying the extent of spatial autocorrelation in disease rating, Phytophthora rubi DNA concentrations in roots, Pratylenchus penetrans densities in roots and soil, soil texture, and elevation in four commercial red raspberry production fields in Oregon (OR-1 and OR-2) and Washington (WA-1 and WA-2).
| Field | Variables | Modela | Nuggetb | Sillc | Ranged |
|---|---|---|---|---|---|
| OR-1 | Disease rating | Gaussian | 0.01 | 0.02 | 102.27 |
| P. rubi DNA in root | Gaussian | 1.05 | 0.44 | 100.72 | |
| P. penetrans in root | Gaussian | 0.50 | 0.03 | 29.52 | |
| P. penetrans in soil | Gaussian | 0.76 | 0.11 | 50.01 | |
| Sand | Exponential | 0.002 | 0.003 | 625.91 | |
| Silt | Exponential | 0.001 | 0.003 | 983.76 | |
| Clay | Gaussian | 0.001 | 0.0005 | 73.70 | |
| Elevation | Gaussian | 0.002 | 0.41 | 107.19 | |
| OR-2 | Disease rating | Exponential | 0.004 | 0.004 | 644.08 |
| P. rubi DNA in root | Gaussian | 0.54 | 0.03 | 36.47 | |
| P. penetrans in root | Exponential | 1.62 | 1.17 | 674.35 | |
| P. penetrans in soil | Exponential | 0 | 0.39 | 10.03 | |
| Sand | Gaussian | 0.004 | 0.002 | 72.89 | |
| Silt | Exponential | 0.003 | 0.004 | 105.97 | |
| Clay | Gaussian | 0.001 | 0.0007 | 56.90 | |
| Elevation | Exponential | 0.044 | 0.15 | 861.29 | |
| WA-1 | Disease rating | Gaussian | 0.03 | 0.32 | 439.20 |
| P. rubi DNA in root | Exponential | 0.37 | 1.98 | 37.66 | |
| P. penetrans in root | Spherical | 0.31 | 0.14 | 48.26 | |
| P. penetrans in soil | Spherical | 0.08 | 0.56 | 94.31 | |
| Sand | Spherical | 0.003 | 0.004 | 505.74 | |
| Silt | Gaussian | 0.003 | 0.002 | 75.60 | |
| Clay | Exponential | 0.001 | 0.0004 | 145.25 | |
| Elevation | Gaussian | 0.024 | 104.36 | 2,855.12 | |
| WA-2 | Disease rating | Exponential | 0.0005 | 0.09 | 265.02 |
| P. rubi DNA in root | Exponential | 0.89 | 0.89 | 362.76 | |
| P. penetrans in root | Exponential | 0.62 | 0.74 | 23.00 | |
| P. penetrans in soil | Exponential | 0.13 | 0.42 | 49.90 | |
| Sand | Gaussian | 0.002 | 0.004 | 59.61 | |
| Silt | Exponential | 0.002 | 0.006 | 82.70 | |
| Clay | Exponential | 0 | 0.002 | 79.82 | |
| Elevation | Gaussian | 0.01 | 0.10 | 96.70 |

Figure 8:
Directional experimental variogram graph for assessing potential directional variations in the spatial structure of disease rating, Phytophthora rubi DNA concentrations in roots, and Pratylenchus penetrans densities in roots and soil in four commercial red raspberry production fields in Oregon (OR-1 and OR-2) and Washington (WA-1 and WA-2). Directional angles used for the graph include 0° (North–South), 45° (Northeast–Southwest), 90° (East–West), and 135° (Southeast–Northwest). The overlapping of all the angle point lines indicates no directional variations in the spatial structure of the attribute values (isotropy), while major gaps between the angle point lines indicate the presence of directional trends (anisotropy).

Figure 9:
Directional experimental variogram graph for assessing potential directional variations in the spatial structure of soil texture (sand, silt, and clay) and field elevation in four commercial red raspberry production fields in Oregon (OR-1 and OR-2) and Washington (WA-1 and WA-2). Directional angles used for the graph include 0° (North–South), 45° (Northeast–Southwest), 90° (East–West), and 135° (Southeast–Northwest). The overlapping of all the angle point lines indicates no directional variations in the spatial structure of the attribute values (isotropy), while major gaps between the angle point lines indicate the presence of directional trends (anisotropy).

Figure 10:
Kriging density graph for comparing the distribution of interpolated values of disease rating, Phytophthora rubi DNA concentrations in roots, and Pratylenchus penetrans densities in roots and soil across four commercial red raspberry production fields in Oregon (OR-1 and OR-2) and Washington (WA-1 and WA-2). The x-axis shows the attribute values of the variable, and the y-axis shows the proportion value assigned to each range of the attribute values.

Figure 11:
Kriging density graph for comparing the distribution of interpolated values of soil texture (sand, silt, and clay) and field elevation across four commercial red raspberry production fields in Oregon (OR-1 and OR-2) and Washington (WA-1 and WA-2). The x-axis shows the attribute values of the variable, and the y-axis shows the proportion value assigned to each range of the attribute values.

Figure 12:
Spatial distribution of disease rating across four commercial red raspberry production fields in Oregon (OR-1 and OR-2) and Washington (WA-1 and WA-2). The ordinary kriging was used as a probabilistic interpolator to predict disease ratings at one or more unsampled points. Northing divides the map from north to south and Easting from west to east. Northing and Easting are grid references and are expressed in meters.

Figure 13:
Spatial distribution of Phytophthora rubi DNA concentrations in roots across four commercial red raspberry production fields in Oregon (OR-1 and OR-2) and Washington (WA-1 and WA-2). The ordinary kriging was used as a probabilistic interpolator to predict P. rubi DNA in roots at one or more unsampled points. Northing divides the map from north to south and Easting from west to east. Northing and Easting are grid references and are expressed in meters.

Figure 14:
Spatial distribution of Pratylenchus penetrans densities in roots across four commercial red raspberry production fields in Oregon (OR-1 and OR-2) and Washington (WA-1 and WA-2). The ordinary kriging was used as a probabilistic interpolator to predict P. penetrans densities in roots at one or more unsampled points. Northing divides the map from north to south and Easting from west to east. Northing and Easting are grid references and are expressed in meters.

Figure 15:
Spatial distribution of Pratylenchus penetrans densities in soil across four commercial red raspberry production fields in Oregon (OR-1 and OR-2) and Washington (WA-1 and WA-2). The ordinary kriging was used as a probabilistic interpolator to predict P. penetrans in the soil at one or more unsampled points. Northing divides the map from north to south and Easting from west to east. Northing and Easting are grid references and are expressed in meters.

Figure 16:
Spatial distribution of the percentage of sand across four commercial red raspberry production fields in Oregon (OR-1 and OR-2) and Washington (WA-1 and WA-2). The ordinary kriging was used as a probabilistic interpolator to predict the percentage of sand at one or more unsampled points. Northing divides the map from north to south and Easting from west to east. Northing and Easting are grid references and are expressed in meters.

Figure 17:
Spatial distribution of the percentage of silt across four commercial red raspberry production fields in Oregon (OR-1 and OR-2) and Washington (WA-1 and WA-2). The ordinary kriging was used as a probabilistic interpolator to predict the percentage of silt at one or more unsampled points. Northing divides the map from north to south and Easting from west to east. Northing and Easting are grid references and are expressed in meters.

Figure 18:
Spatial distribution of the percentage of clay across four commercial red raspberry production fields in Oregon (OR-1 and OR-2) and Washington (WA-1 and WA-2). The ordinary kriging was used as a probabilistic interpolator to predict the percentage of clay at one or more unsampled points. Northing divides the map from north to south and Easting from west to east. Northing and Easting are grid references and are expressed in meters.

Figure 19:
Spatial distribution of field elevation across four commercial red raspberry production fields in Oregon (OR-1 and OR-2) and Washington (WA-1 and WA-2). The ordinary kriging was used as a probabilistic interpolator to predict field elevation at one or more unsampled points. Northing divides the map from north to south and Easting from west to east. Northing and Easting are grid references and are expressed in meters.
Table 4:
Coefficient estimates and SE for the OLS, SLM, SDM, SEM, CAR, and SARMA multiple regression models and associated VIF and P values for Phytophthora rubi DNA concentrations in roots regressed against soil texture (sand, silt, and clay) and elevation in four commercial red raspberry production fields in Oregon (OR-1 and OR-2) and Washington (WA-1 and WA-2).
| Field | Variablesa | OLS | SLM | SDM | SEM | CAR | SARMA | |||||||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Estimate | SE | P | VIF | Model | Estimate | SE | P | Model | Estimate | SE | P | Model | Estimate | SE | P | Model | Estimate | SE | P | Model | Estimate | SE | P | Model | ||
| OR-1 | Intercept | 170.82 | 176.79 | 0.34 | … | … | 162.61 | 168.89 | 0.34 | … | 630.02 | 1,137.13 | 0.58 | … | 206.50 | 171.30 | 0.23 | … | 165.21 | 169.63 | 0.33 | … | 352.59 | 174.37 | 0.04 | … |
| Sand | −90.38 | 93.71 | 0.34 | 834 | … | −86.08 | 89.52 | 0.34 | … | −58.62 | 85.97 | 0.50 | … | −109.83 | 90.71 | 0.23 | … | −87.16 | 89.91 | 0.33 | … | −190.22 | 91.85 | 0.04 | … | |
| Silt | −106.57 | 106.04 | 0.32 | 672 | … | −101.50 | 101.30 | 0.32 | …. | −69.18 | 97.38 | 0.48 | …. | −129.10 | 102.67 | 0.21 | …. | −103.13 | 101.73 | 0.31 | …. | −219.04 | 104.35 | 0.04 | …. | |
| Clay | −71.96 | 84.94 | 0.40 | 371 | …. | −68.82 | 81.13 | 0.40 | …. | −43.99 | 78.40 | 0.57 | …. | −86.67 | 82.50 | 0.29 | …. | −69.55 | 81.53 | 0.39 | …. | −150.11 | 84.75 | 0.08 | …. | |
| Elevation | 0.14 | 0.21 | 0.52 | 1 | …. | 0.14 | 0.21 | 0.51 | …. | −0.27 | 0.56 | 0.63 | …. | 0.18 | 0.16 | 0.26 | …. | 0.12 | 0.20 | 0.55 | …. | 0.34 | 0.07 | <0.001 | …. | |
| P | …. | …. | …. | …. | 0.12 | …. | …. | …. | 0.61 | …. | …. | …. | 0.002 | …. | …. | …. | 0.52 | …. | …. | …. | 0.81 | …. | …. | …. | <0.001 | |
| R2 | …. | …. | …. | …. | 0.12 | …. | …. | …. | 0.13 | …. | …. | …. | 0.31 | …. | …. | …. | 0.13 | …. | …. | …. | 0.12 | …. | …. | …. | 0.27 | |
| ρ | …. | …. | …. | …. | …. | …. | …. | …. | 0.16 | …. | …. | …. | −1.61 | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | |
| λ | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | −0.45 | …. | …. | …. | −0.11 | …. | …. | …. | −1.00 | |
| AIC | …. | …. | …. | …. | 188.75 | …. | …. | …. | 190.52 | …. | …. | …. | 184.66 | …. | …. | …. | 190.33 | …. | …. | …. | 190.69 | …. | …. | …. | 179.81 | |
| OR-2 | Intercept | 3.57 | 5.96 | 0.55 | …. | …. | 3.77 | 5.69 | 0.51 | …. | 64.68 | 34.00 | 0.06 | …. | 3.71 | 5.71 | 0.52 | …. | 3.81 | 5.71 | 0.50 | …. | 3.75 | 5.71 | 0.51 | …. |
| Sand | −3.33 | 3.36 | 0.33 | 7 | …. | −3.35 | 3.21 | 0.30 | …. | −4.27 | 2.96 | 0.15 | …. | −3.29 | 3.21 | 0.30 | …. | −3.31 | 3.21 | 0.30 | …. | −3.25 | 3.20 | 0.31 | …. | |
| Silt | −1.35 | 2.73 | 0.62 | 4 | …. | −1.39 | 2.61 | 0.59 | …. | −0.90 | 2.37 | 0.71 | …. | −1.35 | 2.62 | 0.61 | …. | −1.33 | 2.62 | 0.61 | …. | −1.33 | 2.62 | 0.61 | …. | |
| Clay | −1.74 | 4.84 | 0.72 | 4 | …. | −1.95 | 4.63 | 0.67 | …. | −4.48 | 4.31 | 0.30 | …. | −2.11 | 4.64 | 0.65 | …. | −2.24 | 4.64 | 0.63 | …. | −2.28 | 4.65 | 0.62 | …. | |
| Elevation | 0.70 | 0.43 | 0.11 | 1 | …. | 0.72 | 0.41 | 0.08 | …. | 0.99 | 0.43 | 0.02 | …. | 0.74 | 0.41 | 0.07 | …. | 0.71 | 0.41 | 0.08 | …. | 0.77 | 0.41 | 0.06 | …. | |
| P | …. | …. | …. | …. | 0.20 | …. | …. | …. | 0.66 | …. | …. | …. | 0.08 | …. | …. | …. | 0.75 | …. | …. | …. | 0.80 | …. | …. | …. | 0.70 | |
| R2 | …. | …. | …. | …. | 0.10 | …. | …. | …. | 0.10 | …. | …. | …. | 0.26 | …. | …. | …. | 0.10 | …. | …. | …. | 0.10 | …. | …. | …. | 0.10 | |
| ρ | …. | …. | …. | …. | …. | …. | …. | …. | −0.19 | …. | …. | …. | −0.95 | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | |
| λ | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | −0.16 | …. | …. | …. | −0.21 | …. | …. | …. | −0.22 | |
| AIC | …. | …. | …. | …. | 140.22 | …. | …. | …. | 142.03 | …. | …. | …. | 138.41 | …. | …. | …. | 142.12 | …. | …. | …. | 142.16 | …. | …. | …. | 142.07 | |
| WA-1 | Intercept | 377.42 | 178.96 | 0.04 | …. | …. | 366.48 | 171.24 | 0.03 | …. | 2,253.52 | 928.36 | 0.02 | …. | 433.58 | 172.67 | 0.01 | …. | 394.63 | 172.45 | 0.02 | …. | 623.12 | 168.46 | <0.001 | …. |
| Sand | −234.25 | 110.15 | 0.04 | 2,273 | …. | −227.56 | 105.39 | 0.03 | …. | −307.03 | 109.63 | 0.01 | …. | −269.09 | 106.27 | 0.01 | …. | −245.12 | 106.14 | 0.02 | …. | −385.75 | 103.65 | <0.001 | …. | |
| Silt | −216.77 | 102.23 | 0.04 | 1,513 | …. | −210.62 | 97.81 | 0.03 | …. | −283.21 | 101.50 | 0.01 | …. | −249.03 | 98.70 | 0.01 | …. | −226.96 | 98.56 | 0.02 | …. | −359.67 | 96.37 | <0.001 | …. | |
| Clay | −136.93 | 69.69 | 0.05 | 234 | …. | −132.92 | 66.68 | 0.05 | …. | −182.98 | 69.40 | 0.01 | …. | −157.58 | 67.22 | 0.02 | …. | −142.08 | 67.14 | 0.03 | …. | −226.26 | 65.59 | <0.001 | …. | |
| Elevation | 0.16 | 0.59 | 0.79 | 2 | …. | 0.23 | 0.59 | 0.70 | …. | 0.61 | 0.96 | 0.53 | …. | 0.16 | 0.53 | 0.76 | …. | 0.14 | 0.54 | 0.80 | …. | 0.03 | 0.47 | 0.95 | …. | |
| P | …. | …. | …. | …. | 0.06 | …. | …. | …. | 0.79 | …. | …. | …. | 0.32 | …. | …. | …. | 0.56 | …. | …. | …. | 0.64 | …. | …. | …. | <0.001 | |
| R2 | …. | …. | …. | …. | 0.15 | …. | …. | …. | 0.15 | …. | …. | …. | 0.26 | …. | …. | …. | 0.16 | …. | …. | …. | 0.16 | …. | …. | …. | 0.33 | |
| ρ | …. | …. | …. | …. | …. | …. | …. | …. | 0.10 | …. | …. | …. | −0.56 | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | |
| λ | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | −0.35 | …. | …. | …. | −0.47 | …. | …. | …. | −1.00 | |
| AIC | …. | …. | …. | …. | 205.23 | …. | …. | …. | 207.16 | …. | …. | …. | 207.30 | …. | …. | …. | 206.89 | …. | …. | …. | 207.01 | …. | …. | …. | 192.91 | |
| WA-2 | Intercept | 31.13 | 81.32 | 0.70 | …. | …. | 55.75 | 74.27 | 0.45 | …. | −1,283.90 | 435.02 | 0.003 | …. | 81.42 | 72.40 | 0.26 | …. | 73.91 | 75.04 | 0.32 | …. | 81.12 | 68.18 | 0.23 | …. |
| Sand | −13.68 | 46.87 | 0.77 | 918 | …. | −29.74 | 42.81 | 0.49 | …. | 1.43 | 45.08 | 0.97 | …. | −44.84 | 41.77 | 0.28 | …. | −39.77 | 43.26 | 0.36 | …. | −45.34 | 39.32 | 0.25 | …. | |
| Silt | −20.09 | 48.30 | 0.68 | 740 | …. | −35.34 | 44.11 | 0.42 | …. | −3.13 | 46.18 | 0.95 | …. | −50.61 | 43.02 | 0.24 | …. | −46.71 | 44.59 | 0.29 | …. | −50.56 | 40.54 | 0.21 | …. | |
| Clay | −14.28 | 35.07 | 0.69 | 150 | …. | −22.02 | 32.03 | 0.49 | …. | 7.21 | 33.75 | 0.83 | …. | −31.23 | 31.03 | 0.31 | …. | −29.04 | 32.27 | 0.37 | …. | −29.98 | 29.13 | 0.30 | …. | |
| Elevation | 0.22 | 0.41 | 0.60 | 1 | …. | 0.07 | 0.38 | 0.86 | …. | 0.36 | 0.66 | 0.58 | …. | 0.21 | 0.55 | 0.71 | …. | 0.47 | 0.49 | 0.34 | …. | 0.30 | 0.59 | 0.61 | …. | |
| P | …. | …. | …. | …. | 0.01 | …. | …. | …. | 0.04 | …. | …. | …. | 0.72 | …. | …. | …. | 0.05 | …. | …. | …. | 0.16 | …. | …. | …. | 0.01 | |
| R2 | …. | …. | …. | …. | 0.21 | …. | …. | …. | 0.26 | …. | …. | …. | 0.39 | …. | …. | …. | 0.26 | …. | …. | …. | 0.24 | …. | …. | …. | 0.29 | |
| ρ | …. | …. | …. | …. | …. | …. | …. | …. | 0.56 | …. | …. | …. | −0.17 | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | |
| λ | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | 0.70 | …. | …. | …. | 0.76 | …. | …. | …. | 1.82 | |
| AIC | …. | …. | …. | …. | 174.41 | …. | …. | …. | 172.22 | …. | …. | …. | 168.70 | …. | …. | …. | 172.43 | …. | …. | …. | 174.42 | …. | …. | …. | 170.42 | |
a Independent variables were sand, silt, clay, and field elevation. The P value represents the significance of the model at P < 0.05. R2 is the Nagelkerke pseudo-R-squared; ρ is a fitting parameter for SLM and SDM; λ is a fitting parameter for SEM, CAR, and SARMA. AIC was used to compare OLS, SLM, SDM, SEM, CAR, and SARMA models and determine the best model that fits the data for each field. The lower the AIC, the better the model.
Table 5:
Coefficient estimates and SE for the OLS, SLM, SDM, SEM, CAR, and SARMA multiple regression models and associated VIF and P values for Pratylenchus penetrans densites in roots regressed against soil texture (sand, silt, and clay) and elevation in four commercial red raspberry production fields in Oregon (OR-1 and OR-2) and Washington (WA-1 and WA-2).
| Field | Variablesa | OLS | SLM | SDM | SEM | CAR | SARMA | |||||||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Estimate | SE | P | VIF | Model | Estimate | SE | P | Model | Estimate | SE | P | Model | Estimate | SE | P | Model | Estimate | SE | P | Model | Estimate | SE | P | Model | ||
| OR-1 | Intercept | 22.66 | 119.13 | 0.85 | …. | …. | 22.73 | 114.06 | 0.84 | …. | 973.21 | 805.65 | 0.23 | …. | 29.70 | 115.29 | 0.80 | …. | 28.07 | 114.95 | 0.80 | …. | −0.03 | 111.84 | 0.99 | …. |
| Sand | −12.03 | 63.15 | 0.85 | 834 | …. | −12.05 | 60.46 | 0.84 | …. | −57.46 | 62.92 | 0.36 | …. | −15.45 | 61.03 | 0.80 | …. | −14.49 | 60.60 | 0.81 | …. | 1.24 | 58.91 | 0.98 | …. | |
| Silt | −10.88 | 71.46 | 0.88 | 672 | …. | −10.86 | 68.42 | 0.87 | …. | −62.92 | 71.27 | 0.38 | …. | −14.67 | 69.08 | 0.83 | …. | −13.61 | 68.92 | 0.84 | …. | 3.39 | 66.93 | 0.96 | …. | |
| Clay | −14.89 | 57.24 | 0.80 | 371 | …. | −15.03 | 54.80 | 0.78 | …. | −55.89 | 57.40 | 0.33 | …. | −19.50 | 55.57 | 0.73 | …. | −18.83 | 55.31 | 0.73 | …. | −6.89 | 54.35 | 0.90 | …. | |
| Elevation | 0.10 | 0.14 | 0.50 | 1 | …. | 0.11 | 0.14 | 0.44 | …. | −0.34 | 0.41 | 0.42 | …. | 0.12 | 0.10 | 0.22 | …. | 0.09 | 0.12 | 0.46 | …. | 0.15 | 0.05 | 0.002 | …. | |
| P | …. | …. | …. | …. | 0.37 | …. | …. | …. | 0.87 | …. | …. | …. | 0.14 | …. | …. | …. | 0.35 | …. | …. | …. | 0.52 | …. | …. | …. | <0.001 | |
| R2 | …. | …. | …. | …. | 0.07 | …. | …. | …. | 0.07 | …. | …. | …. | 0.18 | …. | …. | …. | 0.09 | …. | …. | …. | 0.08 | …. | …. | …. | 0.31 | |
| ρ | …. | …. | …. | …. | …. | …. | …. | …. | −0.07 | …. | …. | …. | −0.88 | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | |
| λ | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | −0.60 | …. | …. | …. | −0.58 | …. | …. | …. | −0.99 | |
| AIC | …. | …. | …. | …. | 141.38 | …. | …. | …. | 143.35 | …. | …. | …. | 143.80 | …. | …. | …. | 142.50 | …. | …. | …. | 142.96 | …. | …. | …. | 125.53 | |
| OR-2 | Intercept | 3.49 | 10.82 | 0.75 | …. | …. | 3.60 | 10.36 | 0.73 | …. | 25.86 | 63.55 | 0.68 | …. | 3.27 | 10.36 | 0.75 | …. | 3.77 | 10.36 | 0.72 | …. | 3.34 | 10.35 | 0.75 | …. |
| Sand | 0.35 | 6.10 | 0.95 | 7 | …. | 0.44 | 5.84 | 0.94 | …. | −1.02 | 5.62 | 0.86 | …. | 0.83 | 5.81 | 0.89 | …. | 0.60 | 5.83 | 0.92 | …. | 1.23 | 5.76 | 0.83 | …. | |
| Silt | −3.42 | 4.96 | 0.49 | 4 | …. | −3.41 | 4.74 | 0.47 | …. | −3.60 | 4.49 | 0.42 | …. | −3.35 | 4.76 | 0.48 | …. | −3.38 | 4.75 | 0.48 | …. | −3.45 | 4.77 | 0.47 | …. | |
| Clay | 1.80 | 8.80 | 0.84 | 4 | …. | 1.71 | 8.42 | 0.84 | …. | −0.04 | 8.11 | 0.99 | …. | 1.55 | 8.43 | 0.85 | …. | 0.99 | 8.43 | 0.91 | …. | 1.10 | 8.46 | 0.90 | …. | |
| Elevation | −0.92 | 0.79 | 0.25 | 1 | …. | −0.90 | 0.75 | 0.23 | …. | −1.18 | 0.80 | 0.14 | …. | −0.88 | 0.74 | 0.24 | …. | −0.94 | 0.75 | 0.21 | …. | −0.88 | 0.72 | 0.22 | …. | |
| P | …. | …. | …. | …. | 0.49 | …. | …. | …. | 0.80 | …. | …. | …. | 0.19 | …. | …. | …. | 0.66 | …. | …. | …. | 0.77 | …. | …. | …. | 0.51 | |
| R2 | …. | …. | …. | …. | 0.06 | …. | …. | …. | 0.06 | …. | …. | …. | 0.17 | …. | …. | …. | 0.06 | …. | …. | …. | 0.06 | …. | …. | …. | 0.07 | |
| ρ | …. | …. | …. | …. | …. | …. | …. | …. | −0.10 | …. | …. | …. | −0.64 | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | |
| λ | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | −0.22 | …. | …. | …. | −0.18 | …. | …. | …. | −0.43 | |
| AIC | …. | …. | …. | …. | 211.88 | …. | …. | …. | 213.82 | …. | …. | …. | 214.17 | …. | …. | …. | 213.68 | …. | …. | …. | 213.80 | …. | …. | …. | 213.44 | |
| WA-1 | Intercept | −76.26 | 100.24 | 0.45 | …. | …. | −77.12 | 95.99 | 0.42 | …. | 179.96 | 501.46 | 0.72 | …. | −76.26 | 96.02 | 0.43 | …. | −76.81 | 96.01 | 0.42 | …. | −76.27 | 96.05 | 0.43 | …. |
| Sand | 46.61 | 61.70 | 0.45 | 2,272 | …. | 47.17 | 59.08 | 0.42 | …. | 36.20 | 62.66 | 0.56 | …. | 46.62 | 59.10 | 0.43 | …. | 46.94 | 59.09 | 0.43 | …. | 46.62 | 59.12 | 0.43 | …. | |
| Silt | 44.13 | 57.26 | 0.44 | 1,513 | …. | 44.59 | 54.83 | 0.42 | …. | 33.18 | 58.03 | 0.57 | …. | 44.12 | 54.85 | 0.42 | …. | 44.43 | 54.84 | 0.42 | …. | 44.11 | 54.87 | 0.42 | …. | |
| Clay | 29.62 | 39.04 | 0.45 | 234 | …. | 30.00 | 37.38 | 0.42 | …. | 22.51 | 39.73 | 0.57 | …. | 29.63 | 37.39 | 0.43 | …. | 29.86 | 37.39 | 0.42 | …. | 29.64 | 37.41 | 0.43 | …. | |
| Elevation | 0.39 | 0.33 | 0.24 | 2 | …. | 0.40 | 0.32 | 0.22 | …. | 0.23 | 0.56 | 0.68 | …. | 0.39 | 0.32 | 0.21 | …. | 0.39 | 0.32 | 0.21 | …. | 0.39 | 0.32 | 0.21 | …. | |
| P | …. | …. | …. | …. | 0.58 | …. | …. | …. | 0.88 | …. | …. | …. | 0.57 | …. | …. | …. | 0.98 | …. | …. | …. | 0.99 | …. | …. | …. | 0.97 | |
| R2 | …. | …. | …. | …. | 0.05 | …. | …. | …. | 0.05 | …. | …. | …. | 0.12 | …. | …. | …. | 0.05 | …. | …. | …. | 0.05 | …. | …. | …. | 0.05 | |
| ρ | …. | …. | …. | …. | …. | …. | …. | …. | −0.07 | …. | …. | …. | −0.25 | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | |
| λ | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | −0.01 | …. | …. | …. | −0.02 | …. | …. | …. | −0.02 | |
| AIC | …. | …. | …. | …. | 135.68 | …. | …. | …. | 137.66 | …. | …. | …. | 141.14 | …. | …. | …. | 137.68 | …. | …. | …. | 137.68 | …. | …. | …. | 137.68 | |
| WA-2 | Intercept | −69.62 | 92.71 | 0.46 | …. | …. | −80.33 | 88.63 | 0.36 | …. | −555.77 | 494.67 | 0.26 | …. | −85.09 | 83.81 | 0.31 | …. | −105.32 | 88.00 | 0.23 | …. | −102.97 | 81.30 | 0.20 | …. |
| Sand | 42.80 | 53.43 | 0.43 | 918 | …. | 49.75 | 51.18 | 0.33 | …. | 49.42 | 51.62 | 0.34 | …. | 52.09 | 48.36 | 0.28 | …. | 63.01 | 50.72 | 0.21 | …. | 62.42 | 46.93 | 0.18 | …. | |
| Silt | 43.95 | 55.07 | 0.43 | 740 | …. | 50.55 | 52.68 | 0.34 | …. | 52.80 | 52.88 | 0.32 | …. | 52.72 | 49.63 | 0.29 | …. | 65.84 | 52.22 | 0.21 | …. | 63.45 | 48.10 | 0.19 | …. | |
| Clay | 23.00 | 39.98 | 0.57 | 150 | …. | 26.83 | 38.16 | 0.48 | …. | 31.98 | 38.73 | 0.41 | …. | 29.20 | 36.41 | 0.42 | …. | 37.54 | 38.05 | 0.32 | …. | 36.09 | 35.40 | 0.31 | …. | |
| Elevation | 0.81 | 0.47 | 0.09 | 1 | …. | 1 | 0.47 | 0.03 | …. | 0.24 | 0.77 | 0.75 | …. | 1.04 | 0.26 | <0.001 | …. | 0.81 | 0.37 | 0.03 | …. | 1.19 | 0.17 | <0.001 | …. | |
| P | …. | …. | …. | …. | 0.03 | …. | …. | …. | 0.45 | …. | …. | …. | 0.02 | …. | …. | …. | 0.04 | …. | …. | …. | 0.23 | …. | …. | …. | <0.001 | |
| R2 | …. | …. | …. | …. | 0.18 | …. | …. | …. | 0.19 | …. | …. | …. | 0.29 | …. | …. | …. | 0.24 | …. | …. | …. | 0.20 | …. | …. | …. | 0.42 | |
| ρ | …. | …. | …. | …. | …. | …. | …. | …. | −0.29 | …. | …. | …. | −1.29 | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | |
| λ | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | −1.25 | …. | …. | …. | −0.87 | …. | …. | …. | −0.99 | |
| AIC | …. | …. | …. | …. | 190.14 | …. | …. | …. | 191.57 | …. | …. | …. | 191.06 | …. | …. | …. | 187.75 | …. | …. | …. | 190.73 | …. | …. | …. | 170.95 | |
a Independent variables were sand, silt, clay, and field elevation. The P value represents the significance of the model at P < 0.05. R2 is the Nagelkerke pseudo-R-squared; ρ is a fitting parameter for SLM and SDM; λ is a fitting parameter for SEM, CAR, and SARMA. AIC was used to compare OLS, SLM, SDM, SEM, CAR, and SARMA models and determine the best model that fits the data for each field. The lower the AIC, the better the model.
Table 6:
Coefficient estimates and SE for the OLS, SLM, SDM, SEM, CAR, and SARMA multiple regression models and associated VIF and P values for Pratylenchus penetrans in soil regressed against soil texture (sand, silt, and clay) and elevation in four commercial red raspberry production fields in Oregon (OR-1 and OR-2) and Washington (WA-1 and WA-2).
| Field | Variablesa | OLS | SLM | SDM | SEM | CAR | SARMA | |||||||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Estimate | SE | P | VIF | Model | Estimate | SE | P | Model | Estimate | SE | P | Model | Estimate | SE | P | Model | Estimate | SE | P | Model | Estimate | SE | P | Model | ||
| OR-1 | Intercept | −36.41 | 148.53 | 0.80 | …. | …. | −37.35 | 142.21 | 0.79 | …. | 1,044.05 | 848.43 | 0.22 | …. | −68.40 | 143.65 | 0.63 | …. | −52.73 | 143.26 | 0.71 | …. | −71.80 | 144.06 | 0.62 | …. |
| Sand | 19.96 | 78.73 | 0.80 | 834 | …. | 20.50 | 75.38 | 0.78 | …. | −70.87 | 63.18 | 0.26 | …. | 38.28 | 76.03 | 0.61 | …. | 29.76 | 75.90 | 0.69 | …. | 39.88 | 76.26 | 0.60 | …. | |
| Silt | 25.04 | 89.09 | 0.78 | 672 | …. | 25.66 | 85.30 | 0.76 | …. | −78.09 | 71.53 | 0.27 | …. | 45.24 | 86.07 | 0.60 | …. | 35.89 | 85.89 | 0.68 | …. | 47.07 | 86.33 | 0.59 | …. | |
| Clay | 12.55 | 71.36 | 0.86 | 371 | …. | 12.91 | 68.32 | 0.85 | …. | −70.68 | 57.59 | 0.22 | …. | 24.91 | 69.27 | 0.72 | …. | 17.65 | 68.94 | 0.80 | …. | 27.04 | 69.43 | 0.70 | …. | |
| Elevation | 0.13 | 0.18 | 0.48 | 1 | …. | 0.13 | 0.18 | 0.46 | …. | 0.82 | 0.42 | 0.05 | …. | 0.06 | 0.12 | 0.61 | …. | 0.04 | 0.15 | 0.77 | …. | 0.08 | 0.12 | 0.53 | …. | |
| P | …. | …. | …. | …. | 0.36 | …. | …. | …. | 0.92 | …. | …. | …. | <0.001 | …. | …. | …. | 0.31 | …. | …. | …. | 0.48 | …. | …. | …. | 0.37 | |
| R2 | …. | …. | …. | …. | 0.07 | …. | …. | …. | 0.07 | …. | …. | …. | 0.42 | …. | …. | …. | 0.09 | …. | …. | …. | 0.08 | …. | …. | …. | 0.09 | |
| ρ | …. | …. | …. | …. | …. | …. | …. | …. | −0.03 | …. | …. | …. | −1.95 | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | |
| λ | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | −0.67 | …. | …. | …. | −0.60 | …. | …. | …. | −0.43 | |
| AIC | …. | …. | …. | …. | 167.85 | …. | …. | …. | 169.84 | …. | …. | …. | 149.76 | …. | …. | …. | 168.8 | …. | …. | …. | 169.35 | …. | …. | …. | 169.04 | |
| OR-2 | Intercept | 0.34 | 5.17 | 0.95 | …. | …. | −0.45 | 4.92 | 0.93 | …. | 15.33 | 31.00 | 0.62 | …. | −0.02 | 4.87 | 0.99 | …. | 0.03 | 4.94 | 0.99 | …. | −0.01 | 4.88 | 0.99 | …. |
| Sand | 0.76 | 2.92 | 0.80 | 7 | …. | 0.87 | 2.76 | 0.75 | …. | −0.32 | 2.74 | 0.91 | …. | 0.82 | 2.77 | 0.77 | …. | 0.69 | 2.79 | 0.80 | …. | 0.79 | 2.77 | 0.78 | …. | |
| Silt | −0.36 | 2.37 | 0.88 | 4 | …. | −0.15 | 2.24 | 0.94 | …. | −1.28 | 2.21 | 0.56 | …. | −0.02 | 2.22 | 0.99 | …. | −0.34 | 2.26 | 0.88 | …. | −0.01 | 2.23 | 0.99 | …. | |
| Clay | 3.04 | 4.20 | 0.47 | 4 | …. | 3.13 | 3.98 | 0.43 | …. | 1.99 | 3.95 | 0.61 | …. | 3.10 | 3.96 | 0.43 | …. | 3.60 | 4.01 | 0.37 | …. | 3.13 | 3.97 | 0.43 | …. | |
| Elevation | −0.53 | 0.38 | 0.16 | 1 | …. | −0.49 | 0.36 | 0.16 | …. | −0.84 | 0.40 | 0.03 | …. | −0.49 | 0.36 | 0.18 | …. | −0.49 | 0.36 | 0.18 | …. | −0.50 | 0.36 | 0.17 | …. | |
| P | …. | …. | …. | …. | 0.64 | …. | …. | …. | 0.32 | …. | …. | …. | 0.95 | …. | …. | …. | 0.35 | …. | …. | …. | 0.69 | …. | …. | …. | 0.37 | |
| R2 | …. | …. | …. | …. | 0.04 | …. | …. | …. | 0.06 | …. | …. | …. | 0.14 | …. | …. | …. | 0.06 | …. | …. | …. | 0.05 | …. | …. | …. | 0.06 | |
| ρ | …. | …. | …. | …. | …. | …. | …. | …. | 0.29 | …. | …. | …. | −0.03 | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | |
| λ | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | 0.30 | …. | …. | …. | 0.11 | …. | …. | …. | 0.34 | |
| AIC | …. | …. | …. | …. | 123.25 | …. | …. | …. | 124.26 | …. | …. | …. | 126.93 | …. | …. | …. | 124.40 | …. | …. | …. | 125.09 | …. | …. | …. | 124.45 | |
| WA-1 | Intercept | 30.66 | 99.00 | 0.76 | …. | …. | 13.45 | 86.71 | 0.88 | …. | 2,135.04 | 424.48 | <0.001 | …. | −33.96 | 86.30 | 0.69 | …. | −4.70 | 90.26 | 0.96 | …. | −58.12 | 84.84 | 0.49 | …. |
| Sand | −17.59 | 60.93 | 0.77 | 2,273 | …. | −7.27 | 53.37 | 0.89 | …. | −140.67 | 52.15 | 0.007 | …. | 21.97 | 53.10 | 0.68 | …. | 4.29 | 55.54 | 0.93 | …. | 37.00 | 52.21 | 0.48 | …. | |
| Silt | −17.61 | 56.55 | 0.76 | 1,513 | …. | −7.56 | 49.53 | 0.88 | …. | −132.37 | 48.37 | 0.006 | …. | 19.72 | 49.16 | 0.69 | …. | 2.66 | 51.48 | 0.96 | …. | 33.30 | 48.34 | 0.49 | …. | |
| Clay | −15.32 | 38.55 | 0.69 | 234 | …. | −8.53 | 33.77 | 0.80 | …. | −93.85 | 33.09 | 0.004 | …. | 10.04 | 33.65 | 0.77 | …. | −2.33 | 35.17 | 0.95 | …. | 19.54 | 33.11 | 0.55 | …. | |
| Elevation | 0.68 | 0.33 | 0.04 | 2 | …. | 0.22 | 0.30 | 0.47 | …. | −0.63 | 0.44 | 0.15 | …. | 0.38 | 0.39 | 0.33 | …. | 0.49 | 0.35 | 0.16 | …. | 0.45 | 0.37 | 0.22 | …. | |
| P | …. | …. | …. | …. | <0.001 | …. | …. | …. | 0.004 | …. | …. | …. | 0.96 | …. | …. | …. | 0.02 | …. | …. | …. | 0.07 | …. | …. | …. | 0.02 | |
| R2 | …. | …. | …. | …. | 0.29 | …. | …. | …. | 0.38 | …. | …. | …. | 0.59 | …. | …. | …. | 0.35 | …. | …. | …. | 0.32 | …. | …. | …. | 0.35 | |
| ρ | …. | …. | …. | …. | …. | …. | …. | …. | 0.70 | …. | …. | …. | −0.02 | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | |
| λ | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | 0.72 | …. | …. | …. | 0.77 | …. | …. | …. | 1.01 | |
| AIC | …. | …. | …. | …. | 134.18 | …. | …. | …. | 127.78 | …. | …. | …. | 111.71 | …. | …. | …. | 130.76 | …. | …. | …. | 133.03 | …. | …. | …. | 130.58 | |
| WA-2 | Intercept | −60.06 | 53.39 | 0.26 | …. | …. | −51.53 | 49.99 | 0.30 | …. | 157.38 | 292.91 | 0.59 | …. | −52.72 | 49.96 | 0.29 | …. | −55.47 | 50.96 | 0.28 | …. | −40.27 | 49.21 | 0.41 | …. |
| Sand | 36.21 | 30.77 | 0.24 | 918 | …. | 30.52 | 28.82 | 0.29 | …. | 5.95 | 30.84 | 0.85 | …. | 31.58 | 28.80 | 0.27 | …. | 33.65 | 29.37 | 0.25 | …. | 24.24 | 28.37 | 0.39 | …. | |
| Silt | 38.69 | 31.71 | 0.23 | 740 | …. | 32.91 | 29.70 | 0.27 | …. | 9.24 | 31.60 | 0.77 | …. | 34.22 | 29.69 | 0.25 | …. | 35.80 | 30.27 | 0.24 | …. | 26.65 | 29.25 | 0.36 | …. | |
| Clay | 22.07 | 23.02 | 0.34 | 150 | …. | 18.93 | 21.55 | 0.38 | …. | 3.47 | 23.16 | 0.88 | …. | 20.09 | 21.48 | 0.35 | …. | 20.22 | 21.96 | 0.36 | …. | 15.37 | 21.12 | 0.47 | …. | |
| Elevation | −0.03 | 0.27 | 0.92 | 1 | …. | −0.04 | 0.25 | 0.87 | …. | −0.39 | 0.46 | 0.39 | …. | −0.11 | 0.32 | 0.73 | …. | 0.003 | 0.27 | 0.99 | …. | −0.12 | 0.34 | 0.73 | …. | |
| P | …. | …. | …. | …. | 0.08 | …. | …. | …. | 0.17 | …. | …. | …. | 0.74 | …. | …. | …. | 0.38 | …. | …. | …. | 0.71 | …. | …. | …. | 0.24 | |
| R2 | …. | …. | …. | …. | 0.15 | …. | …. | …. | 0.17 | …. | …. | …. | 0.25 | …. | …. | …. | 0.16 | …. | …. | …. | 0.15 | …. | …. | …. | 0.16 | |
| ρ | …. | …. | …. | …. | …. | …. | …. | …. | 0.45 | …. | …. | …. | 0.14 | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | |
| λ | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | 0.42 | …. | …. | …. | 0.15 | …. | …. | …. | 0.83 | |
| AIC | …. | …. | …. | …. | 123.91 | …. | …. | …. | 124.05 | …. | …. | …. | 126.10 | …. | …. | …. | 125.13 | …. | …. | …. | 125.77 | …. | …. | …. | 124.55 | |
a Independent variables were sand, silt, clay, and field elevation. The P value represents the significance of the model at P < 0.05. R2 is the Nagelkerke pseudo-R-squared; ρ is a fitting parameter for SLM and SDM; λ is a fitting parameter for SEM, CAR, and SARMA. AIC was used to compare OLS, SLM, SDM, SEM, CAR, and SARMA models and determine the best model that fits the data for each field. The lower the AIC, the better the model.
Table 7:
Coefficient estimates and SE for the OLS, SLM, SDM, SEM, CAR, and SARMA multiple regression models and associated VIF and P values for disease rating regressed against Phytophthora rubi DNA in roots, Pratylenchus penetrans in roots and soil in four commercial red raspberry production fields in Oregon (OR-1 and OR-2) and Washington (WA-1 and WA-2).
| Field | Variablesa | OLS | SLM | SDM | SEM | CAR | SARMA | |||||||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Estimate | SE | P | VIF | Model | Estimate | SE | P | Model | Estimate | SE | P | Model | Estimate | SE | P | Model | Estimate | SE | P | Model | Estimate | SE | P | Model | ||
| OR-1 | Intercept | 0.83 | 0.03 | <0.001 | …. | …. | 0.20 | 0.14 | 0.15 | …. | 0.78 | 0.34 | 0.02 | …. | 0.83 | 0.05 | <0.001 | …. | 0.82 | 0.03 | <0.001 | …. | 0.83 | 0.05 | <0.001 | …. |
| P. rubi DNA | 0.08 | 0.01 | <0.001 | 1.02 | …. | 0.07 | 0.01 | <0.001 | …. | 0.07 | 0.01 | <0.001 | …. | 0.07 | 0.01 | <0.001 | …. | 0.09 | 0.01 | <0.001 | …. | 0.07 | 0.01 | <0.001 | …. | |
| P. penetrans (root) | 0.01 | 0.02 | 0.57 | 1.30 | …. | 0.01 | 0.02 | 0.52 | …. | 0.02 | 0.02 | 0.20 | …. | 0.01 | 0.02 | 0.62 | …. | 0.01 | 0.02 | 0.71 | …. | 0.01 | 0.02 | 0.66 | …. | |
| P. penetrans (soil) | −0.04 | 0.02 | 0.04 | 1.32 | …. | −0.02 | 0.02 | 0.15 | …. | −0.03 | 0.02 | 0.10 | …. | −0.02 | 0.02 | 0.19 | …. | −0.03 | 0.02 | 0.04 | …. | −0.01 | 0.01 | 0.42 | …. | |
| P | …. | …. | …. | …. | <0.001 | …. | …. | …. | <0.001 | …. | …. | …. | 0.79 | …. | …. | …. | <0.001 | …. | …. | …. | 0.56 | …. | …. | …. | <0.001 | |
| R2 | …. | …. | …. | …. | 0.46 | …. | …. | …. | 0.57 | …. | …. | …. | 0.61 | …. | …. | …. | 0.53 | …. | …. | …. | 0.46 | …. | …. | …. | 0.56 | |
| ρ | …. | …. | …. | …. | …. | …. | …. | …. | 0.67 | …. | …. | …. | −0.12 | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | |
| λ | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | 0.73 | …. | …. | …. | 0.09 | …. | …. | …. | 2.06 | |
| AIC | …. | …. | …. | …. | −84.58 | …. | …. | …. | −95.82 | …. | …. | …. | −96.37 | …. | …. | …. | −90.26 | …. | …. | …. | −82.92 | …. | …. | …. | −95.25 | |
| OR-2 | Intercept | 0.61 | 0.02 | <0.001 | …. | …. | 0.58 | 0.23 | 0.01 | …. | 0.74 | 0.25 | 0.003 | …. | 0.61 | 0.02 | <0.001 | …. | 0.61 | 0.02 | <0.001 | …. | 0.61 | 0.02 | <0.001 | …. |
| P. rubi DNA | 0.01 | 0.01 | 0.27 | 1.01 | …. | 0.01 | 0.01 | 0.25 | …. | 0.006 | 0.01 | 0.56 | …. | 0.01 | 0.01 | 0.25 | …. | 0.01 | 0.01 | 0.26 | …. | 0.01 | 0.01 | 0.25 | …. | |
| P. penetrans (root) | 0.008 | 0.006 | 0.22 | 1.09 | …. | 0.008 | 0.006 | 0.21 | …. | 0.01 | 0.006 | 0.08 | …. | 0.008 | 0.006 | 0.18 | …. | 0.008 | 0.006 | 0.19 | …. | 0.008 | 0.006 | 0.18 | …. | |
| P. penetrans (soil) | 0.01 | 0.01 | 0.38 | 1.09 | …. | 0.01 | 0.01 | 0.36 | …. | 0.004 | 0.01 | 0.74 | …. | 0.01 | 0.01 | 0.35 | …. | 0.01 | 0.01 | 0.35 | …. | 0.01 | 0.01 | 0.34 | …. | |
| P | …. | …. | …. | …. | 0.21 | …. | …. | …. | 0.88 | …. | …. | …. | 0.58 | …. | …. | …. | 0.81 | …. | …. | …. | 0.95 | …. | …. | …. | 0.77 | |
| R2 | …. | …. | …. | …. | 0.08 | …. | …. | …. | 0.08 | …. | …. | …. | 0.17 | …. | …. | …. | 0.08 | …. | …. | …. | 0.08 | …. | …. | …. | 0.08 | |
| ρ | …. | …. | …. | …. | …. | …. | …. | …. | 0.05 | …. | …. | …. | −0.24 | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | |
| λ | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | −0.10 | …. | …. | …. | −0.01 | …. | …. | …. | −0.13 | |
| AIC | …. | …. | …. | …. | −153.46 | …. | …. | …. | −151.48 | …. | …. | …. | −152.09 | …. | …. | …. | −151.52 | …. | …. | …. | −151.47 | …. | …. | …. | −151.54 | |
| WA-1 | Intercept | 0.59 | 0.03 | <0.001 | …. | …. | 0.31 | 0.13 | 0.01 | …. | 0.82 | 0.27 | 0.003 | …. | 0.58 | 0.04 | <0.001 | …. | 0.59 | 0.03 | <0.001 | …. | 0.58 | 0.04 | <0.001 | …. |
| P. rubi DNA | 0.09 | 0.01 | <0.001 | 1.00 | …. | 0.08 | 0.01 | <0.001 | …. | 0.08 | 0.01 | <0.001 | …. | 0.08 | 0.01 | <0.001 | …. | 0.09 | 0.01 | <0.001 | …. | 0.08 | 0.01 | <0.001 | …. | |
| P. penetrans (root) | −0.01 | 0.03 | 0.63 | 1.01 | …. | −0.008 | 0.02 | 0.74 | …. | −0.02 | 0.02 | 0.48 | …. | −0.009 | 0.02 | 0.74 | …. | −0.01 | 0.03 | 0.59 | …. | −0.008 | 0.02 | 0.73 | …. | |
| P. penetrans (soil) | −0.05 | 0.02 | 0.03 | 1.01 | …. | −0.03 | 0.02 | 0.18 | …. | −0.02 | 0.03 | 0.51 | …. | −0.04 | 0.02 | 0.11 | …. | −0.05 | 0.02 | 0.04 | …. | −0.038 | 0.03 | 0.14 | …. | |
| P | …. | …. | …. | …. | <0.001 | …. | …. | …. | 0.04 | …. | …. | …. | 0.36 | …. | …. | …. | 0.35 | …. | …. | …. | 0.83 | …. | …. | …. | 0.28 | |
| R2 | …. | …. | …. | …. | 0.43 | …. | …. | …. | 0.46 | …. | …. | …. | 0.51 | …. | …. | …. | 0.43 | …. | …. | …. | 0.43 | …. | …. | …. | 0.44 | |
| ρ | …. | …. | …. | …. | …. | …. | …. | …. | 0.44 | …. | …. | …. | −0.48 | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | |
| λ | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | 0.38 | …. | …. | …. | 0.04 | …. | …. | …. | 0.63 | |
| AIC | …. | …. | …. | …. | −54.35 | …. | …. | …. | −56.27 | …. | …. | …. | −55.19 | …. | …. | …. | −53.22 | …. | …. | …. | −52.40 | …. | …. | …. | −53.52 | |
| WA-2 | Intercept | 0.53 | 0.05 | <0.001 | …. | …. | 0.09 | 0.09 | 0.27 | …. | 0.47 | 0.18 | 0.009 | …. | 0.59 | 0.09 | <0.001 | …. | 0.57 | 0.05 | <0.001 | …. | 0.62 | 0.06 | <0.001 | …. |
| P. rubi DNA | 0.12 | 0.01 | <0.001 | 1.07 | …. | 0.08 | 0.01 | <0.001 | …. | 0.08 | 0.01 | <0.001 | …. | 0.08 | 0.01 | <0.001 | …. | 0.12 | 0.01 | <0.001 | …. | 0.08 | 0.01 | <0.001 | …. | |
| P. penetrans (root) | 0.01 | 0.01 | 0.44 | 1.14 | …. | −0.009 | 0.01 | 0.39 | …. | −0.01 | 0.01 | 0.22 | …. | −0.009 | 0.01 | 0.40 | …. | 0.01 | 0.01 | 0.44 | …. | −0.01 | 0.01 | 0.20 | …. | |
| P. penetrans (soil) | 0.07 | 0.02 | 0.006 | 1.08 | …. | 0.04 | 0.02 | 0.02 | …. | 0.05 | 0.02 | 0.009 | …. | 0.05 | 0.02 | 0.01 | …. | 0.04 | 0.02 | 0.08 | …. | 0.07 | 0.02 | <0.001 | …. | |
| P | …. | …. | …. | …. | <0.001 | …. | …. | …. | <0.001 | …. | …. | …. | 0.60 | …. | …. | …. | <0.001 | …. | …. | …. | 0.18 | …. | …. | …. | <0.001 | |
| R2 | …. | …. | …. | …. | 0.57 | …. | …. | …. | 0.70 | …. | …. | …. | 0.73 | …. | …. | …. | 0.68 | …. | …. | …. | 0.58 | …. | …. | …. | 0.68 | |
| ρ | …. | …. | …. | …. | …. | …. | …. | …. | 0.67 | …. | …. | …. | 0.20 | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | |
| λ | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | 0.84 | …. | …. | …. | 0.31 | …. | …. | …. | 2.06 | |
| AIC | …. | …. | …. | …. | −76.74 | …. | …. | …. | −97.91 | …. | …. | …. | −98.44 | …. | …. | …. | −92.92 | …. | …. | …. | −76.50 | …. | …. | …. | −93.94 | |
a Independent variables were P. rubi DNA concentrations in roots and P. penetrans in roots and soil. The P value represents the significance of the model at P < 0.05. R2 is the Nagelkerke pseudo-R-squared; ρ is a fitting parameter for SLM and SDM; λ is a fitting parameter for SEM, CAR, and SARMA. AIC was used to compare OLS, SLM, SDM, SEM, CAR, and SARMA models and determine the best model that fits the data for each field. The lower the AIC, the better the model.
Table 8:
Coefficient estimates and SE for the OLS, SLM, SDM, SEM, CAR, and SARMA multiple regression models and associated VIF and P values for Pratylenchus penetrans densities in roots regressed against P. penetrans densities in soil and Phytophthora rubi DNA concentrations in roots in four commercial red raspberry production fields in Oregon (OR-1 and OR-2) and Washington (WA-1 and WA-2).
| Field | Variablesa | OLS | SLM | SDM | SEM | CAR | SARMA | |||||||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Estimate | SE | P | VIF | Model | Estimate | SE | P | Model | Estimate | SE | P | Model | Estimate | SE | P | Model | Estimate | SE | P | Model | Estimate | SE | P | Model | ||
| OR-1 | Intercept | 0.11 | 0.19 | 0.59 | …. | …. | 0.05 | 0.26 | 0.84 | …. | −1.19 | 1.28 | 0.35 | …. | 0.10 | 0.19 | 0.60 | …. | 0.11 | 0.19 | 0.57 | …. | 0.09 | 0.19 | 0.62 | …. |
| P. penetrans (soil) | 0.39 | 0.09 | <0.001 | 1.02 | …. | 0.38 | 0.09 | <0.001 | …. | 0.42 | 0.10 | <0.001 | …. | 0.39 | 0.09 | <0.001 | …. | 0.39 | 0.09 | <0.001 | …. | 0.40 | 0.09 | <0.001 | …. | |
| P. rubi DNA | 0.02 | 0.08 | 0.82 | 1.02 | …. | 0.02 | 0.07 | 0.79 | …. | 0.06 | 0.08 | 0.46 | …. | 0.02 | 0.07 | 0.83 | …. | 0.01 | 0.07 | 0.87 | …. | 0.02 | 0.07 | 0.83 | …. | |
| P | …. | …. | …. | …. | <0.001 | …. | …. | …. | 0.75 | …. | …. | …. | 0.56 | …. | …. | …. | 0.83 | …. | …. | …. | 0.85 | …. | …. | …. | 0.75 | |
| R2 | …. | …. | …. | …. | 0.23 | …. | …. | …. | 0.23 | …. | …. | …. | 0.25 | …. | …. | …. | 0.23 | …. | …. | …. | 0.23 | …. | …. | …. | 0.23 | |
| ρ | …. | …. | …. | …. | …. | …. | …. | …. | 0.11 | …. | …. | …. | −0.27 | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | |
| λ | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | −0.10 | …. | …. | …. | −0.14 | …. | …. | …. | −0.18 | |
| AIC | …. | …. | …. | …. | 126.36 | …. | …. | …. | 128.26 | …. | …. | …. | 130.39 | …. | …. | …. | 128.32 | …. | …. | …. | 128.33 | …. | …. | …. | 128.26 | |
| OR-2 | Intercept | 0.32 | 0.48 | 0.52 | …. | …. | 0.55 | 0.70 | 0.43 | …. | −3.38 | 1.69 | 0.04 | …. | 0.19 | 0.44 | 0.66 | …. | 0.07 | 0.44 | 0.86 | …. | −0.09 | 0.25 | 0.72 | …. |
| P. penetrans (soil) | 0.59 | 0.7 | 0.03 | 1.0 | …. | 0.60 | 0.26 | 0.02 | …. | 0.64 | 0.25 | 0.01 | …. | 0.64 | 0.25 | 0.01 | …. | 0.69 | 0.25 | 0.005 | …. | 0.71 | 0.11 | <0.001 | …. | |
| P. rubi DNA | 0.10 | 0.22 | 0.67 | 1.0 | …. | 0.10 | 0.22 | 0.63 | …. | 0.26 | 0.21 | 0.22 | …. | 0.14 | 0.22 | 0.49 | …. | 0.15 | 0.22 | 0.49 | …. | 0.39 | 0.21 | 0.06 | …. | |
| P | …. | …. | …. | …. | 0.08 | …. | …. | …. | 0.61 | …. | …. | …. | 0.09 | …. | …. | …. | 0.36 | …. | …. | …. | 0.35 | …. | …. | …. | <0.001 | |
| R2 | …. | …. | …. | …. | 0.08 | …. | …. | …. | 0.09 | …. | …. | …. | 0.17 | …. | …. | …. | 0.09 | …. | …. | …. | 0.09 | …. | …. | …. | 0.33 | |
| ρ | …. | …. | …. | …. | …. | …. | …. | …. | −0.21 | …. | …. | …. | −0.85 | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | |
| λ | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | −0.44 | …. | …. | …. | −1.02 | …. | …. | …. | −0.99 | |
| AIC | …. | …. | …. | …. | 206.40 | …. | …. | …. | 208.14 | …. | …. | …. | 206.19 | …. | …. | …. | 207.56 | …. | …. | …. | 207.53 | …. | …. | …. | 189.57 | |
| WA-1 | Intercept | 0.48 | 0.14 | 0.001 | …. | …. | 0.51 | 0.25 | 0.04 | …. | −0.03 | 0.43 | 0.94 | …. | 0.46 | 0.13 | <0.001 | …. | 0.48 | 0.13 | <0.001 | …. | 0.45 | 0.12 | <0.001 | …. |
| P. penetrans (soil) | 0.09 | 0.12 | 0.42 | 1.0 | …. | 0.10 | 0.11 | 0.38 | …. | −0.04 | 0.15 | 0.81 | …. | 0.11 | 0.11 | 0.30 | …. | 0.09 | 0.11 | 0.42 | …. | 0.12 | 0.10 | 0.22 | …. | |
| P. rubi DNA | −0.01 | 0.07 | 0.85 | 1.0 | …. | −0.01 | 0.07 | 0.85 | …. | −0.006 | 0.07 | 0.93 | …. | −0.01 | 0.07 | 0.87 | …. | −0.01 | 0.07 | 0.88 | …. | −0.01 | 0.06 | 0.87 | …. | |
| P | …. | …. | …. | …. | 0.71 | …. | …. | …. | 0.88 | …. | …. | …. | 0.69 | …. | …. | …. | 0.72 | …. | …. | …. | 0.78 | …. | …. | …. | 0.65 | |
| R2 | …. | …. | …. | …. | 0.01 | …. | …. | …. | 0.01 | …. | …. | …. | 0.06 | …. | …. | …. | 0.01 | …. | …. | …. | 0.01 | …. | …. | …. | 0.01 | |
| ρ | …. | …. | …. | …. | …. | …. | …. | …. | −0.06 | …. | …. | …. | −0.17 | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | |
| λ | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | −0.17 | …. | …. | …. | −0.21 | …. | …. | …. | −0.27 | |
| AIC | …. | …. | …. | …. | 134.05 | …. | …. | …. | 136.03 | …. | …. | …. | 137.17 | …. | …. | …. | 135.92 | …. | …. | …. | 135.97 | …. | …. | …. | 135.84 | |
| WA-2 | Intercept | 0.80 | 0.49 | 0.11 | …. | …. | 0.61 | 0.73 | 0.40 | …. | 1.06 | 1.35 | 0.43 | …. | 0.59 | 0.43 | 0.18 | …. | 0.69 | 0.47 | 0.14 | …. | 0.70 | 0.46 | 0.13 | …. |
| P. penetrans (soil) | 0.47 | 0.22 | 0.04 | 1.0 | …. | 0.45 | 0.22 | 0.04 | …. | 0.34 | 0.21 | 0.10 | …. | 0.52 | 0.20 | 0.01 | …. | 0.53 | 0.21 | 0.01 | …. | 0.50 | 0.21 | 0.02 | …. | |
| P. rubi DNA | 0.26 | 0.14 | 0.06 | 1.0 | …. | 0.24 | 0.14 | 0.08 | …. | 0.08 | 0.14 | 0.58 | …. | 0.36 | 0.12 | 0.003 | …. | 0.26 | 0.13 | 0.05 | …. | 0.31 | 0.13 | 0.02 | …. | |
| P | …. | …. | …. | …. | 0.03 | …. | …. | …. | 0.66 | …. | …. | …. | 0.06 | …. | …. | …. | 0.51 | …. | …. | …. | 0.71 | …. | …. | …. | 0.66 | |
| R2 | …. | …. | …. | …. | 0.12 | …. | …. | …. | 0.12 | …. | …. | …. | 0.29 | …. | …. | …. | 0.13 | …. | …. | …. | 0.12 | …. | …. | …. | 0.12 | |
| ρ | …. | …. | …. | …. | …. | …. | …. | …. | 0.13 | …. | …. | …. | −0.82 | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | |
| λ | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | …. | −0.40 | …. | …. | …. | −0.24 | …. | …. | …. | −0.16 | |
| AIC | …. | …. | …. | …. | 190.27 | …. | …. | …. | 192.08 | …. | …. | …. | 183.53 | …. | …. | …. | 191.85 | …. | …. | …. | 192.14 | …. | …. | …. | 192.08 | |
a Independent variables were P. rubi DNA concentrations in roots and P. penetrans in soil. The P value represents the significance of the model at P < 0.05. R2 is the Nagelkerke pseudo-R-squared; ρ is a fitting parameter for SLM and SDM; λ is a fitting parameter for SEM, CAR, and SARMA. AIC was used to compare OLS, SLM, SDM, SEM, CAR, and SARMA models and determine the best model that fits the data for each field. The lower the AIC, the better the model.
Table S1:
Global Moran’s I test for spatial autocorrelation in the residuals for Phytophthora rubi DNA concentrations in roots, Pratylenchus penetrans densites in root and soil regressed against soil texture (sand, silt, and clay), and field elevation in four commercial red raspberry production fields in Oregon (OR-1 and OR-2) and Washington (WA-1 and WA-2).
| Field | Predicted | Moran’s I coefficienta | P-valueb |
|---|---|---|---|
| OR-1 | P. rubi DNA in root | −0.018 | 0.29 |
| P. penetrans in root | −0.026 | 0.39 | |
| P. penetrans in soil | −0.030 | 0.45 | |
| OR-2 | P. rubi DNA in root | −0.011 | 0.39 |
| P. penetrans in root | −0.016 | 0.44 | |
| P. penetrans in soil | 0.046 | 0.03 | |
| WA-1 | P. rubi DNA in root | −0.017 | 0.36 |
| P. penetrans in root | −0.001 | 0.19 | |
| P. penetrans in soil | 0.100 | <0.001 | |
| WA-2 | P. rubi DNA in root | 0.064 | <0.001 |
| P. penetrans in root | −0.060 | 0.78 | |
| P. penetrans in soil | 0.030 | 0.01 |
Table S2:
Global Moran’s I test for spatial autocorrelation in the residuals for visual disease rating regressed against Phytophthora rubi DNA concentrations in roots and Pratylenchus penetrans densities in roots and soil in four commercial red raspberry production fields in Oregon (OR-1 and OR-2) and Washington (WA-1 and WA-2).
Table S3:
Global Moran’s I test for spatial autocorrelation in the residuals for Pratylenchus penetrans densities in root regressed against P. penetrans densities in soil and Phytophthora rubi DNA concentrations in roots in four commercial red raspberry production fields in Oregon (OR-1 and OR-2) and Washington (WA-1 and WA-2).