g.l. rees, g.s. pettygrove , and r.j. southard methods, including some non - laboratory analysis: 16...

1
Measuring potassium uptake and growth response of Measuring potassium uptake and growth response of annual ryegrass at multiple K rates in K-fixing and non-K-fixing soils annual ryegrass at multiple K rates in K-fixing and non-K-fixing soils G.L. Rees, G.S. Pettygrove, and R.J. Southard INTRODUCTION METHODS G.L. Rees, G.S. Pettygrove, and R.J. Southard Department of Land, Air & Water Resources, INTRODUCTION The fixation of potassium in non-exchangeable forms has been identified as a source of concern for soil METHODS Soils Soil samples used from six pedons at two depths each from vineyard Department of Land, Air & Water Resources, University of California, Davis has been identified as a source of concern for soil fertility management in parts of the San Joaquin Valley of central California. The potential for K fixation in Soil samples used from six pedons at two depths each from vineyard and almond orchard sites from across the San Joaquin Valley Soil properties are shown in Table 1. Total yield by K rate of central California. The potential for K fixation in these soils has been linked to vermiculite in the silt and fine sand fraction of granitic alluvium 1 . Applying K Soil properties are shown in Table 1. Pot experiment 14 16 Total yield by K rate a a a a a a a a b b a a ab c and fine sand fraction of granitic alluvium . Applying K to K-fixing soils at rates equivalent to measured K fixation potential values resulted in much of the K Pot experiment 1kg soil plus 1kg washed quartz sand mixed with soluble and control release N and P sources, plus K treatments 12 14 (g) a a a a a a a a b b ab c being removed from ammonium acetate- exchangeable K (XK) pool within 24 hours, but without K rates of 0, 50, 250, and 1000 mg/kg soil applied as K 2 SO 4 , with four replicates for each soil/K rate treatment 8 10 Yield a a a b Fig. 2. Visual K deficiency symptoms in annual satiating the K-fixing capacity of the soils 2 . Increasing K additions resulted in increasing quantities of K fixed. Annual ryegrass (Lolium multiflorum) seeded at 1.5 g per pot and grown in greenhouse Grass harvested by clipping at 1 cm above the soil surface at 3, 6, 4 6 Fig. 2. Visual K deficiency symptoms in annual ryegrass grown in soil VSS E 100-120 with no K added nine weeks after germination. (3 rd clipping) The sodium tetraphenylboron method of K extraction (TPB-K), developed by Scott et al. 3 and refined by Cox Grass harvested by clipping at 1 cm above the soil surface at 3, 6, and 9 weeks after germination Oven-dry above ground biomass (“yield”) and tissue K measured 4 VSS E 0- 20 VSS E 100-120 DH 2 0- 20 DH 2 40- 60 KTR A 0- 20 KTR A 40-60 (TPB-K), developed by Scott et al. 3 and refined by Cox et al. 4 has been shown to extract more K than traditional methods, including some non- Oven-dry above ground biomass (“yield”) and tissue K measured Laboratory analysis: 16 a a a a c traditional methods, including some non- exchangeable K, and has been used as an estimate of plant-available K, given its superior correlation to plant Laboratory analysis: Ammonium acetate-extractable K 7 (XK) 2.5-3 g soil saturated and extracted overnight with 1 M NH 4 OAc (pH 7) using a mechanical vacuum extractor 12 14 g) a a a a a a a b c c plant-available K, given its superior correlation to plant uptake 5 . mechanical vacuum extractor K determined by flame emission spectrometry 8 10 Yield (g a a a a a b ab b In an attempt to evaluate the various methods for determining the K status of both K-fixing and non-K- K fixation potential 8 (Kfix) 3 g soil shaken in 30 mL of 2 mM KCl for 1 h Extracted for 30 minutes with 10 mL 4 M NH Cl, and centrifuged 6 8 a a a fixing soils, we conducted a greenhouse pot experiment in twelve diverse soil materials and at four rates of applied K. Annual ryegrass (Lolium Extracted for 30 minutes with 10 mL 4 M NH 4 Cl, and centrifuged K measured by flame emission spectrometry K fixation potential was calculated as the difference between a blank and the 4 DON A 0- 20 DON A 40-60 RM X 0- 20 RM X 40- 60 DOUG 0- 20 DOUG 40-60 rates of applied K. Annual ryegrass (Lolium multiflorum), which is highly efficient at recovering soil K 6 , was grown. Yield and K uptake were measured, and K fixation potential was calculated as the difference between a blank and the measured K solution concentrations Sodium tetraphenylboron-extractable K (TPB-K) 20 40-60 20 60 20 40-60 0 mg/kg soil 50 mg/kg soil 250 mg/kg soil 1000 mg/kg soil K rate: Total yield by K rate for each of the 12 soil materials Fig. 3. Scatterplot matrix comparison of yield and K uptake to K 6 , was grown. Yield and K uptake were measured, and results were compared to laboratory measurements of soil K properties. Sodium tetraphenylboron-extractable K 4 (TPB-K) 1 g soil extracted for 5 minutes with 3 mL of extracting solution (0.2 M NaTPB + 1.7 M NaCl + 0.01 M EDTA) Fig. 1. Total yield by K rate for each of the 12 soil materials used. For each soil, letters indicate significantly different means at the 5% probability level as determined by the comparison of yield and K uptake to laboratory measurements of soil K status. soil K properties. + 1.7 M NaCl + 0.01 M EDTA) Quenched with 25 mL of 0.5 M NH 4 Cl + 0.11 M CuCl 2 Samples heated to boiling for 30-45 minutes to dissolve precipitate K measured by flame emission spectrometry Table 1. Soil properties means at the 5% probability level as determined by the Tukey HSD method. Yield by clipping Depth XK TPB-K TotK Kfix Code Soil/Classification (cm) - - - (mg kg -1 ) - - - K measured by flame emission spectrometry Aqua regia “total K” 9 (TotK) Table 1. Soil properties 2 4 6 8 eld (g) a a a a a a b b c bc ab ab Code Soil/Classification (cm) - - - (mg kg -1 ) - - - VSS E San Joaquin silt loam 0-20 79 189 2100 241 Abruptic Durixeralf 100-120 95 183 3950 632 Aqua regia “total K” (TotK) 0.500 g ball-milled soil digested with aqua regia for 3 hours at 110°C Diluted with 2% nitric acid, filtered, and brought to 250 mL with DI K measured by flame emission spectrometry 0 2 Clipping 1 Clipping 2 Clipping 3 Yie (a) VSS E 100-120cm a Abruptic Durixeralf 100-120 95 183 3950 632 DH 2 Guard clay loam 0-20 194 553 2820 58 Duric Haplaquoll 40-60 116 234 2810 420 K measured by flame emission spectrometry Tissue K 10 (a) VSS E 100-120cm 8 g) a b b b c Duric Haplaquoll 40-60 116 234 2810 420 KTR A Columbia sandy loam 0-20 167 770 4500 -26 Aquic Xerofluvent 40-60 88 300 3940 243 Tissue K Oven-dry grass ground to 40 mesh Extracted for 30 minutes with 2% acetic acid K measured by flame emission spectrometry 0 2 4 6 Yield (g a a a a a a a b b ab Aquic Xerofluvent 40-60 88 300 3940 243 DON A Archerdale clay loam 0-20 269 558 4000 -70 K measured by flame emission spectrometry 0 Clipping 1 Clipping 2 Clipping 3 (b) VSS E 0-20cm a a a Pachic Haploxeroll 40-60 159 234 2840 225 RM X Redding gravelly loam 0-20 87 130 830 -45 DISCUSSION & SUMMARY 2 4 6 8 ield (g) a a a a a a a a a a a a Abruptic Durixeralf 40-60 40 66 880 14 DOUG Vina fine sandy loam 0-20 301 395 1430 -186 1. Cate-Nelson analysis (carried out in R) 11 established critical values for each soil K determination -XK: 167 mg/kg soil 0 2 Clipping 1 Clipping 2 Clipping 3 Yi (c) DH 2 0-20cm Pachic Haploxeroll 40-60 144 155 740 -60 -XK: 167 mg/kg soil -TPB-K: 419 mg/kg soil -TotK: 1663 mg/kg soil 0 mg/kg soil 50 mg/kg soil 250 mg/kg soil 1000 mg/kg soil (c) DH 2 0-20cm K rate: Fig. 4. Yield by clipping for soils (a) VSS E 100-120cm, (b) VSS E 0-20cm, and (c) DH 2 0-20cm. For each -TotK: 1663 mg/kg soil 2. The TPB-K critical value best predicted presence or absence of a Fig. 4. Yield by clipping for soils (a) VSS E 100-120cm, (b) VSS E 0-20cm, and (c) DH 2 0-20cm. For each clipping, letters indicate significantly different means at the 5% probability level by the TukeyHSD method. Photos show no K and 1000 mg/kg soil K treatments for soil VSS E 100-120 cm at the time of the first and third clippings. The high rate lead to greater initial growth, but this was reversed by the K rate (mg/kg soil) Table 2. Ryegrass K uptake 2. The TPB-K critical value best predicted presence or absence of a significant response to additional K, and TPB-K plus added K best correlated with K uptake (Fig. 3) REFERENCES the first and third clippings. The high rate lead to greater initial growth, but this was reversed by the final clipping. K rate (mg/kg soil) Pedon Depth 0 50 250 1000 Code (cm) Total uptake (mg/kg soil) correlated with K uptake (Fig. 3) 3. Soils with initial TPB-K values > 419 mg/kg did not respond to added K, with mixed responses for lower TPB-K soils REFERENCES 1.Murashkina, M.A., R.J. Southard, and G.S. Pettygrove. 2007. Silt and fine sand fractions dominate K fixation in soils derived from granitic alluvium of the San Joaquin Valley, California. Geoderma 141: 283-293. 2. Rees, G.L., G.S. Pettygrove, and R.J. Southard. 2013. Estimating plant-available potassium in potassium-fixing soils. Comm. in Soil Sci. and Plant Anal. 44:741-748. Code (cm) Total uptake (mg/kg soil) VSS E 0-20 239 304 590 1069 VSS E 100-120 340 374 587 747 added K, with mixed responses for lower TPB-K soils 4. High K fixation potential of DH 2 40-60cm expressed in significant 2. Rees, G.L., G.S. Pettygrove, and R.J. Southard. 2013. Estimating plant-available potassium in potassium-fixing soils. Comm. in Soil Sci. and Plant Anal. 44:741-748. 3.Scott, A.D., R. R. Hunziker, and J.J. Hanway. 1960. Chemical extraction of potassium from soils and micaceousminerals with solutions containing sodium tetraphenylboron. I. Preliminary experiments. Soil Sci. Soc. of Am. Proc. 24: 46-51. 4. Cox, A.E., B.C. Joern, and C.B. Roth. 1996. Nonexchangeable ammonium and potassium determination in some Midwestern soils using a dmodifies sodium tetrapheylboron VSS E 100-120 340 374 587 747 DH 2 0-20 558 633 810 957 DH 2 40-60 153 145 348 689 4. High K fixation potential of DH 2 40-60cm expressed in significant response to 1000 mg K/kg soil treatment relative to 250 mg K/kg soil, but high K fixing VSS E 100-120 showed no significant response 4. Cox, A.E., B.C. Joern, and C.B. Roth. 1996. Nonexchangeable ammonium and potassium determination in some Midwestern soils using a dmodifies sodium tetrapheylboron method. Soil Sci. Soc. Am. J. 60:114-120. 5.Cox A.E., B.C. Joern, S.M. Brouder, and D. Gao. 1999. Plant-available potassium assessment with a modified sodium tetraphenylboronmethod. Soil Sci. Soc. Am. J. 63: 902-911. 6. Binet, P., L. el Guessabi, and J. Salette. 1984. The potassium status of soils: significance of the “Italian ryegrass test”. Fertilizer Research 5: 393-402. DH 2 40-60 153 145 348 689 KTR A 0-20 662 679 907 1042 KTR A 40-60 369 452 648 961 soil, but high K fixing VSS E 100-120 showed no significant response to any level of K application 5. Slowly available fixed K not measured by XK or TPB-K method in 6. Binet, P., L. el Guessabi, and J. Salette. 1984. The potassium status of soils: significance of the “Italian ryegrass test”. Fertilizer Research 5: 393-402. 7.Soil Survey Staff. 2004. Soil Survey Laboratory Methods Manual –Soil Survey Investigations Report No. 42. Version 4.0. USDA-NRCS. Lincoln, NE. 8.Murashkina, M., R. J. Southard, and G. S. Pettygrove. 2007. Potassium fixation in San Joaquin Valley soils derived from granitic and nongraniticalluvium. Soil Sci. Soc. Am. J. 71:125-132. KTR A 40-60 369 452 648 961 DON A 0-20 681 774 895 959 DON A 40-60 287 333 519 831 5. Slowly available fixed K not measured by XK or TPB-K method in VSS E 100-120 may have provided K source for low K treatments, evidenced by increased uptake and yield in final clipping relative to 9.RajashekharRao, B.K., J. Bailey, and R.W. Wingwafi. 2011. Comparison of three digestion methods for total soil potassium estimation in soils of Papua New Guinea derived from varying parent materials. Comm. in Soil Sci. and Plant Anal. 42:1259-1265. 10.Miller, R.O. 1998. Extractable chloride, nitrate, orthophosphate, potassium, and sulfate-sulfur in plant tissue: 2% acetic acid extraction. p. 115-118. In Y.P. Kalra(ed.) Handbook of Reference Methods for Plant Analysis. CRC Press, Boca Raton, FL. DON A 40-60 287 333 519 831 RM X 0-20 154 183 435 1043 RM X 40-60 60 126 359 970 evidenced by increased uptake and yield in final clipping relative to high K treatments (Fig. 4) Reference Methods for Plant Analysis. CRC Press, Boca Raton, FL. 11.Mangiafico, S.S. 2013. Cate-Nelson Analysis for BivariateData Using R-project. Journal of Extension 51: Article #5TOT1. URL http://www.joe.org/joe/2013october/tt1.php ACKNOWLEDGEMENTS RM X 40-60 60 126 359 970 DOUG 0-20 324 383 550 791 DOUG 40-60 96 144 325 707 ACKNOWLEDGEMENTS The authors thank Dan Rivers and JiayouDeng for technical assistance. Research was made possible by a grant from the California Department of Food & Agriculture. DOUG 40-60 96 144 325 707

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Measuring potassium uptake and growth response of Measuring potassium uptake and growth response of

annual ryegrass at multiple K rates in K-fixing and non-K-fixing soils annual ryegrass at multiple K rates in K-fixing and non-K-fixing soils G.L. Rees, G.S. Pettygrove, and R.J. Southard

INTRODUCTION METHODS

G.L. Rees, G.S. Pettygrove, and R.J. SouthardDepartment of Land, Air & Water Resources, INTRODUCTION

The fixation of potassium in non-exchangeable forms

has been identified as a source of concern for soil

METHODSSoils

• Soil samples used from six pedons at two depths each from vineyard

Department of Land, Air & Water Resources,

University of California, Davishas been identified as a source of concern for soil

fertility management in parts of the San Joaquin Valley

of central California. The potential for K fixation in

• Soil samples used from six pedons at two depths each from vineyard

and almond orchard sites from across the San Joaquin Valley

• Soil properties are shown in Table 1.Total yield by K rateof central California. The potential for K fixation in

these soils has been linked to vermiculite in the silt

and fine sand fraction of granitic alluvium1. Applying K

• Soil properties are shown in Table 1.

Pot experiment14

16

Total yield by K rate

aa

a a a a

a

a

b

b

aa

ab

c

and fine sand fraction of granitic alluvium . Applying K

to K-fixing soils at rates equivalent to measured K

fixation potential values resulted in much of the K

Pot experiment

• 1kg soil plus 1kg washed quartz sand mixed with soluble and control

release N and P sources, plus K treatments12

14

Yie

ld (

g)

a

a

a

a aa

aa

b

b

ab

c

fixation potential values resulted in much of the K

being removed from ammonium acetate-

exchangeable K (XK) pool within 24 hours, but without

• K rates of 0, 50, 250, and 1000 mg/kg soil applied as K2SO4 , with

four replicates for each soil/K rate treatment

8

10

Yie

ld (

g)

a

aa

b

Fig. 2. Visual K deficiency symptoms in annual satiating the K-fixing capacity of the soils2. Increasing K

additions resulted in increasing quantities of K fixed.

• Annual ryegrass (Lolium multiflorum) seeded at 1.5 g per pot and

grown in greenhouse

• Grass harvested by clipping at 1 cm above the soil surface at 3, 6, 4

6

Fig. 2. Visual K deficiency symptoms in annual

ryegrass grown in soil VSS E 100-120 with no K

added nine weeks after germination. (3rd clipping)

The sodium tetraphenylboron method of K extraction

(TPB-K), developed by Scott et al.3 and refined by Cox

• Grass harvested by clipping at 1 cm above the soil surface at 3, 6,

and 9 weeks after germination

• Oven-dry above ground biomass (“yield”) and tissue K measured

4

VSS E 0-

20

VSS E

100-120

DH 2 0-

20

DH 2 40-

60

KTR A 0-

20

KTR A

40-60

(TPB-K), developed by Scott et al.3 and refined by Cox

et al.4 has been shown to extract more K than

traditional methods, including some non-

• Oven-dry above ground biomass (“yield”) and tissue K measured

Laboratory analysis: 16

aaa

actraditional methods, including some non-

exchangeable K, and has been used as an estimate of

plant-available K, given its superior correlation to plant

Laboratory analysis: Ammonium acetate-extractable K7 (XK)

• 2.5-3 g soil saturated and extracted overnight with 1 M NH4OAc (pH 7) using a

mechanical vacuum extractor 12

14

Yie

ld (

g)

aaa

a

aa

a a

b

c

c

c

plant-available K, given its superior correlation to plant

uptake5. mechanical vacuum extractor

• K determined by flame emission spectrometry

8

10

Yie

ld (

g)

aa

a

aa

b

b

abb

In an attempt to evaluate the various methods for

determining the K status of both K-fixing and non-K-

K fixation potential8 (Kfix)

• 3 g soil shaken in 30 mL of 2 mM KCl for 1 h

• Extracted for 30 minutes with 10 mL 4 M NH Cl, and centrifuged

6

8

a

a

a

determining the K status of both K-fixing and non-K-

fixing soils, we conducted a greenhouse pot

experiment in twelve diverse soil materials and at four

rates of applied K. Annual ryegrass (Lolium

• Extracted for 30 minutes with 10 mL 4 M NH4Cl, and centrifuged

• K measured by flame emission spectrometry

• K fixation potential was calculated as the difference between a blank and the

4

DON A 0-

20

DON A

40-60

RM X 0-

20

RM X 40-

60

DOUG 0-

20

DOUG

40-60rates of applied K. Annual ryegrass (Lolium

multiflorum), which is highly efficient at recovering soil

K6, was grown. Yield and K uptake were measured, and

• K fixation potential was calculated as the difference between a blank and the

measured K solution concentrations

Sodium tetraphenylboron-extractable K (TPB-K)

20 40-60 20 60 20 40-60

0 mg/kg soil 50 mg/kg soil 250 mg/kg soil 1000 mg/kg soil

K rate:

Total yield by K rate for each of the 12 soil materials

Fig. 3. Scatterplot matrix

comparison of yield and K uptake to K6, was grown. Yield and K uptake were measured, and

results were compared to laboratory measurements of

soil K properties.

Sodium tetraphenylboron-extractable K4 (TPB-K)

• 1 g soil extracted for 5 minutes with 3 mL of extracting solution (0.2 M NaTPB

+ 1.7 M NaCl + 0.01 M EDTA)

Fig. 1. Total yield by K rate for each of the 12 soil materials

used. For each soil, letters indicate significantly different

means at the 5% probability level as determined by the

comparison of yield and K uptake to

laboratory measurements of soil K status.

soil K properties. + 1.7 M NaCl + 0.01 M EDTA)

• Quenched with 25 mL of 0.5 M NH4Cl + 0.11 M CuCl2

• Samples heated to boiling for 30-45 minutes to dissolve precipitate

• K measured by flame emission spectrometryTable 1. Soil properties

means at the 5% probability level as determined by the

Tukey HSD method.

Yield by clipping

Depth XK TPB-K TotK Kfix

Code Soil/Classification (cm) - - - (mg kg-1) - - -

• K measured by flame emission spectrometry

Aqua regia “total K”9 (TotK)

Table 1. Soil properties

2

4

6

8

Yie

ld (

g)

Yield by clipping

a

a

a

aaabb

cbc

ab ab

Code Soil/Classification (cm) - - - (mg kg-1) - - -

VSS E San Joaquin silt loam 0-20 79 189 2100 241

Abruptic Durixeralf 100-120 95 183 3950 632

Aqua regia “total K”9 (TotK)

• 0.500 g ball-milled soil digested with aqua regia for 3 hours at 110°C

• Diluted with 2% nitric acid, filtered, and brought to 250 mL with DI

• K measured by flame emission spectrometry

0

2

Clipping 1 Clipping 2 Clipping 3

Yie

ld (

g)

(a) VSS E 100-120cm

a

Abruptic Durixeralf 100-120 95 183 3950 632

DH 2 Guard clay loam 0-20 194 553 2820 58

Duric Haplaquoll 40-60 116 234 2810 420

• K measured by flame emission spectrometry

Tissue K10

(a) VSS E 100-120cm

8

Yie

ld (

g)

ab b

b

c

Duric Haplaquoll 40-60 116 234 2810 420

KTR A Columbia sandy loam 0-20 167 770 4500 -26

Aquic Xerofluvent 40-60 88 300 3940 243

Tissue K

• Oven-dry grass ground to 40 mesh

• Extracted for 30 minutes with 2% acetic acid

• K measured by flame emission spectrometry0

2

4

6

8

Yie

ld (

g)

a

a aa aaa

b bbab

Aquic Xerofluvent 40-60 88 300 3940 243

DON A Archerdale clay loam 0-20 269 558 4000 -70

• K measured by flame emission spectrometry0

Clipping 1 Clipping 2 Clipping 3

(b) VSS E 0-20cmaa a

Pachic Haploxeroll 40-60 159 234 2840 225

RM X Redding gravelly loam 0-20 87 130 830 -45 DISCUSSION & SUMMARY2

4

6

8

Yie

ld (

g)

aaaa

aaaa

aa aa

Abruptic Durixeralf 40-60 40 66 880 14

DOUG Vina fine sandy loam 0-20 301 395 1430 -186

1. Cate-Nelson analysis (carried out in R)11 established critical values

for each soil K determination

-XK: 167 mg/kg soil

0

2

Clipping 1 Clipping 2 Clipping 3

Yie

ld (

g)

(c) DH 2 0-20cmPachic Haploxeroll 40-60 144 155 740 -60 -XK: 167 mg/kg soil

-TPB-K: 419 mg/kg soil

-TotK: 1663 mg/kg soil

0 mg/kg soil 50 mg/kg soil

250 mg/kg soil 1000 mg/kg soil

(c) DH 2 0-20cm

K rate:

Fig. 4. Yield by clipping for soils (a) VSS E 100-120cm, (b) VSS E 0-20cm, and (c) DH 2 0-20cm. For each -TotK: 1663 mg/kg soil

2. The TPB-K critical value best predicted presence or absence of a

Fig. 4. Yield by clipping for soils (a) VSS E 100-120cm, (b) VSS E 0-20cm, and (c) DH 2 0-20cm. For each

clipping, letters indicate significantly different means at the 5% probability level by the Tukey HSD

method. Photos show no K and 1000 mg/kg soil K treatments for soil VSS E 100-120 cm at the time of

the first and third clippings. The high rate lead to greater initial growth, but this was reversed by the K rate (mg/kg soil)

Table 2. Ryegrass K uptake

2. The TPB-K critical value best predicted presence or absence of a

significant response to additional K, and TPB-K plus added K best

correlated with K uptake (Fig. 3)REFERENCES

the first and third clippings. The high rate lead to greater initial growth, but this was reversed by the

final clipping.

K rate (mg/kg soil)

Pedon Depth 0 50 250 1000

Code (cm) Total uptake (mg/kg soil) correlated with K uptake (Fig. 3)

3. Soils with initial TPB-K values > 419 mg/kg did not respond to

added K, with mixed responses for lower TPB-K soils

REFERENCES1. Murashkina, M.A., R.J. Southard, and G.S. Pettygrove. 2007. Silt and fine sand fractions dominate K fixation in soils derived from granitic alluvium of the San Joaquin Valley,

California. Geoderma 141: 283-293.

2. Rees, G.L., G.S. Pettygrove, and R.J. Southard. 2013. Estimating plant-available potassium in potassium-fixing soils. Comm. in Soil Sci. and Plant Anal. 44:741-748.

Code (cm) Total uptake (mg/kg soil)

VSS E 0-20 239 304 590 1069

VSS E 100-120 340 374 587 747added K, with mixed responses for lower TPB-K soils

4. High K fixation potential of DH 2 40-60cm expressed in significant

2. Rees, G.L., G.S. Pettygrove, and R.J. Southard. 2013. Estimating plant-available potassium in potassium-fixing soils. Comm. in Soil Sci. and Plant Anal. 44:741-748.

3. Scott, A.D., R. R. Hunziker, and J.J. Hanway. 1960. Chemical extraction of potassium from soils and micaceous minerals with solutions containing sodium tetraphenylboron. I.

Preliminary experiments. Soil Sci. Soc. of Am. Proc. 24: 46-51.

4. Cox, A.E., B.C. Joern, and C.B. Roth. 1996. Nonexchangeable ammonium and potassium determination in some Midwestern soils using a dmodifies sodium tetrapheylboron

VSS E 100-120 340 374 587 747

DH 2 0-20 558 633 810 957

DH 2 40-60 153 145 348 689 4. High K fixation potential of DH 2 40-60cm expressed in significant

response to 1000 mg K/kg soil treatment relative to 250 mg K/kg

soil, but high K fixing VSS E 100-120 showed no significant response

4. Cox, A.E., B.C. Joern, and C.B. Roth. 1996. Nonexchangeable ammonium and potassium determination in some Midwestern soils using a dmodifies sodium tetrapheylboron

method. Soil Sci. Soc. Am. J. 60:114-120.

5. Cox A.E., B.C. Joern, S.M. Brouder, and D. Gao. 1999. Plant-available potassium assessment with a modified sodium tetraphenylboron method. Soil Sci. Soc. Am. J. 63: 902-911.

6. Binet, P., L. el Guessabi, and J. Salette. 1984. The potassium status of soils: significance of the “Italian ryegrass test”. Fertilizer Research 5: 393-402.

DH 2 40-60 153 145 348 689

KTR A 0-20 662 679 907 1042

KTR A 40-60 369 452 648 961 soil, but high K fixing VSS E 100-120 showed no significant response

to any level of K application

5. Slowly available fixed K not measured by XK or TPB-K method in

6. Binet, P., L. el Guessabi, and J. Salette. 1984. The potassium status of soils: significance of the “Italian ryegrass test”. Fertilizer Research 5: 393-402.

7. Soil Survey Staff. 2004. Soil Survey Laboratory Methods Manual – Soil Survey Investigations Report No. 42. Version 4.0. USDA-NRCS. Lincoln, NE.

8. Murashkina, M., R. J. Southard, and G. S. Pettygrove. 2007. Potassium fixation in San Joaquin Valley soils derived from granitic and nongranitic alluvium. Soil Sci. Soc. Am. J.

71:125-132.

KTR A 40-60 369 452 648 961

DON A 0-20 681 774 895 959

DON A 40-60 287 333 519 8315. Slowly available fixed K not measured by XK or TPB-K method in

VSS E 100-120 may have provided K source for low K treatments,

evidenced by increased uptake and yield in final clipping relative to

9. Rajashekhar Rao, B.K., J. Bailey, and R.W. Wingwafi. 2011. Comparison of three digestion methods for total soil potassium estimation in soils of Papua New Guinea derived from

varying parent materials. Comm. in Soil Sci. and Plant Anal. 42:1259-1265.

10.Miller, R.O. 1998. Extractable chloride, nitrate, orthophosphate, potassium, and sulfate-sulfur in plant tissue: 2% acetic acid extraction. p. 115-118. In Y.P. Kalra (ed.) Handbook of

Reference Methods for Plant Analysis. CRC Press, Boca Raton, FL.

DON A 40-60 287 333 519 831

RM X 0-20 154 183 435 1043

RM X 40-60 60 126 359 970 evidenced by increased uptake and yield in final clipping relative to

high K treatments (Fig. 4)

Reference Methods for Plant Analysis. CRC Press, Boca Raton, FL.

11.Mangiafico, S.S. 2013. Cate-Nelson Analysis for Bivariate Data Using R-project. Journal of Extension 51: Article #5TOT1. URL http://www.joe.org/joe/2013october/tt1.php

ACKNOWLEDGEMENTS

RM X 40-60 60 126 359 970

DOUG 0-20 324 383 550 791

DOUG 40-60 96 144 325 707 ACKNOWLEDGEMENTSThe authors thank Dan Rivers and Jiayou Deng for technical assistance. Research was made possible by a grant from the California Department of Food &

Agriculture.

DOUG 40-60 96 144 325 707