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Published online 25 May 2007
Published in J Environ Qual 36:975-982 (2007)
DOI: 10.2134/jeq2006.0424
© 2007 American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
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Agri-environmental Thresholds using Mehlich III Soil Phosphorus Saturation Index for Vegetables in Histosols

Julie Guérin, Léon-Étienne Parent* and Rahima Abdelhafid

Dep. of Soils and Agri-Food Engineering, Université Laval, Québec, QC, Canada G1K 7P4


Figure 1
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Fig. 1. The r2 values for relationships between the [P/(Al+{gamma}Fe)]M-III ratio as an index of P saturation (IPSM-III) and the degree of P saturation (DPSOX) ({alpha}m = 0.4) or water-extractable P (PW) by varying the {gamma} coefficient in IPSM-III.

 

Figure 2
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Fig. 2. Relationship between the [P/(Al+{gamma}Fe)]M-III ratio as an index of P saturation (IPSM-III) ({gamma} = 5) and the degree of P saturation (DPSOX) ({alpha}m = 0.4).

 

Figure 3
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Fig. 3. Relationship between the [P/(Al+{gamma}Fe)]Mf-III ratio as an index of P saturation (IPSM-III) ({gamma} = 5) and water-extractable P (PW).
 

Figure 4
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Fig. 4. Relationship between relative yield and the [P/(Al+{gamma}Fe)]M-III ratio as an index of P saturation (IPSM-III) ({gamma} = 5) across Group A crops.

 

Figure 5
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Fig. 5. Relationship between relative yield and the [P/(Al+{gamma}Fe)]M-III ratio as an index of P saturation (IPSM-III) ({gamma} = 5) across Group B crops.

 

Figure 6
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Fig. 6. Significance ({alpha} level for rejecting H0) of the partition between two soil groups below or above the [P/(Al+{gamma}Fe)]M-III ratio as an index of P saturation (IPSM-III) separator on the x axis.

 





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