Abstract

Core Ideas: Spatial and seasonal variability in the Illinois soil N test (ISNT)‐N and loss‐on‐ignition (LOI) at 500°C can impact N recommendations. Loss‐on‐ignition determination at 500°C and 360°C are highly correlated. Loss‐on‐ignition and ISNT‐N show strong spatial structure among soils. Soil nitrate sampling is less practical because of its large spatial variability. Intensification of current sampling protocols is needed for LOI and ISNT‐N. The Illinois soil N test (ISNT) with loss‐on‐ignition at 500°C (LOI500) adjustment can identify fields with low versus high soil N supply potential in New York. However, spatial and seasonal variability in ISNT‐N and LOI500 can influence soil N supply classifications. We aimed to determine (i) the influence of sample density on the ratio of ISNT‐N to the critical value for interpretations of ISNT results (ISNT‐NCritical), and N supply classification, (ii) the implications of change in spatial and temporal variability on ISNT‐N interpretations, (iii) the probability of obtaining accurate interpretations as impacted by sampling intensity, and (iv) the influence of using LOI500 equivalents [derived from loss‐on‐ignition at 360°C (LOI360)] on ISNT‐N interpretations. Two 4‐ha silage corn (Zea mays L.) fields were sampled (150 samples per field, 0–20 cm depth; 64 in regular 25 by 25 or 23 by 27 m grids, the remainder in a pattern optimizing lag distance distribution) in July and November. Semivariograms were constructed to investigate spatial dependence. Soil nitrate showed the weakest spatial dependence. Increasing sampling intensity to 3.75 samples ha‐1 reduced the confidence interval for ISNT‐N/ISNT‐NCritical while augmenting the probability (>95%) of obtaining estimates within the true field mean (±6.4%), resulting in consistent classifications. The LOI500 and LOI360 results correlated well (r2 = 0.78); using LOI500 equivalents derived from LOI360 produced identical classifications for 92% of the samples. Effective sampling protocols for ISNT‐N should include sampling at 3.75+ samples ha‐1 for consistent ISNT‐N interpretations, and LOI500 equivalents can be used to derive ISNT‐Ncritical values.

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