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Effects of reduced tillage on vertical phosphorus stratification and availability Clain Jones, Chengci Chen, Evette Allison, and Karnes Neill Montana State.

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Presentation on theme: "Effects of reduced tillage on vertical phosphorus stratification and availability Clain Jones, Chengci Chen, Evette Allison, and Karnes Neill Montana State."— Presentation transcript:

1 Effects of reduced tillage on vertical phosphorus stratification and availability
Clain Jones, Chengci Chen, Evette Allison, and Karnes Neill Montana State University Prepared for 2007 American Society of Agronomy Conference

2 Background Tillage has previously been found to affect available soil P levels (Selles et al. 1999) and vertical P stratification (Grant and Bailey, 1994), yet almost no studies have been conducted on calcareous soils. No research located on effects of CT and NT on P uptake (prior to 2006). Phosphorus uptake and P fertilizer needs could be affected by tillage effects on: 1. P stratification (both vertical and horizontal) 2. Temperature 3. Moisture 4. Nitrogen availability 5. Yield Differences in P stratification and uptake between CT and NT would indicate need for different P rates.

3 Questions 1. Are there differences in vertical stratification of available P between tilled and no-till systems in calcareous soils? 2. Is P uptake different between tillage systems? 3. Should P rates be adjusted for different tillage systems?

4 Materials and Methods Location: Central Ag. Research Ctr., Moccasin, Montana Existing study on tillage, cropping system (fallow, spring wheat, spring pea, winter pea forage  winter wheat), and nitrogen rate (0, 45, 90, 135 kg N/ha) Tillage treatments: 9 year no-till (NTNT) 30+ year CT (CTCT) – Sweep till, 1 pass/year (Reduced T?) NT following CT (CTNT) CT following 9 year no-till (NTCT) P fertilized with the seed (2-2.5 cm deep) each year

5 Study Location

6 Photo: nris.mt.gov

7 Photo: C. Chen, 2007 Spring Wheat Fallow (NTNT) Spring Pea Winter Pea

8 Soil Sampling and Analysis
Fallow soils sampled Sept. 2005 Soil increments: Every 3 cm from 0 to 30 cm Five soils composited per plot (4 replicates) Analyses: Olsen P (top 30 cm) and sequential P fractions (top 15 cm)

9 Sequential Extractions
All in 1:30 soil:water suspensions, shaken 16 h, and centrifuged Resin-P Anion exchange resin capsule, extracted w/ 2M HCl (high availability) Bic-P 0.5 M NaHCO3, pH 8.5 (high availability) NaOH-P 0.1 M NaOH (moderate availability) HCl-P 1 M HCl (low availability)

10 P uptake Tissue P analyzed from winter wheat harvested in 2006 from same plots as soil sampled (90 kg N/ha treatment). Tissue P analyzed in spring pea (grain) and winter pea (forage) harvested in 2007 (0 and 90 kg N/ha in 2006).

11 Results

12 Olsen P Distribution

13 Resin P Distribution

14 (averaged over 0-15 cm depth)
P Fractions (averaged over 0-15 cm depth) b b b a

15 2006 Winter Wheat Aboveground P Uptake
Note: Winter wheat fertilized with 10 kg P/ha

16 2007 Winter Pea Aboveground P Uptake
WP not fertilized. Means of P uptake for 8 subplots per treatment

17 2007 Spring Pea Grain P Uptake
SP not fertilized. Means of P uptake for 8 subplots per treatment.

18 Relevance of P Uptake Our results, combined with research from other recent studies (Lupwayi et al. 2006; Schwab et al. 2006), suggest that P fertilizer rates do not need to be adjusted based on tillage system.

19 Summary Stratification of Olsen P was greater in long-term NT than CT, yet all tillage treatments had much higher P levels near the surface. Long term NT had significantly lower 0.1 M NaOH-P than long term CT (0-15 cm depth). All other P fractions were not significantly different among tillage treatments. Aboveground P uptake was not different among tillage treatments. The results, combined with other recently published studies, suggest that P rate recommendations do not need to consider type of tillage system.

20 Acknowledgments This study was funded by the following:
Montana Fertilizer Advisory Committee

21 QUESTIONS?


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