Effects of Dolomite Source, Dolomite Rate and Fertilizer Rate on Change in pH of Growing Medium Leachate
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C.A. Conover, Ph.D.(1), R.J. Steinkamp(2) and K. Steinkamp(3)
University of Florida
Institute of Food and Agricultural Sciences
Central Florida Research and Education Center
CFREC-Apopka Research Report RH-95-4
A basic ingredient of most potting mixes used in foliage plant production is peat, which tends to be acidic. Dolomite is added to growing medium to raise pH to the range of 5.5 to 6.5 and to supply plants with calcium and magnesium needed for healthy growth. Dolomite also slowly dissolves in the growing medium over time, helping to counteract the acidifying effects some fertilizers and/or irrigation water can have on growing medium pH. The need for new research on pH has been identified by industry as important due to observation of low pH in many soil and water samples.
Nursery supply companies offer several different dolomitic limestone products which vary in particle size (grade). In a previous test, finer grades of limestone were more effective than coarser grades in raising pH of container medium of boxwood (Buxus sempervirens), grown in 2-gal plastic containers over a two year production period (Leda and Wright, 1991).
The following two experiments were performed to explore the short-term effects of different dolomite products having different grades on pH of growing medium in 6-inch (15-cm) pots during production of Dieffenbachia maculata 'Camille'. Whether low pH influences foliage crop quality and whether different dolomite sources could influence pH were the main questions prompting this research. A secondary purpose was to demonstrate effects of using recommended versus excess fertilizer rates on crop quality as well as pH.
For both experiments Dieffenbachia maculata 'Camille' (Camille dieffenbachia, Agristarts II, Inc., Kelly Park Road, Apopka FL 32712) in 72-pack trays were transplanted into 6-inch (15cm) plastic tub pots on June 6, 1994. A customized form of Farard #4 growing medium (Fafard of Florida Inc., 3723 Hogshead Road, Apopka, FL 32703) containing no lime was used. The four different dolomite products incorporated into growing medium at transplanting time were Soil Doctor Dolomite, James River Dolomite, Asgrow Dolomite and James River Camadil Dolomite. The particle size distribution of each of the four products is given in Table 1. 'Camille' dieffenbachia were grown to salable size in a greenhouse where maximum light intensity was about 2000 ft-c (266 µmolm-2s -1) and air temperatures ranged from 65°F to 90°F (18°C to 35°C). Plants were watered overhead one to three times per week as necessary.
Electrical conductivity (µmhos/cm) and pH of leachate collected from growing medium of Camille dieffenbachia were measured when experiments were initiated in June, five days before fertilizer treatments started, then monthly until research was terminated in September, 1994. Plant size index was determined by the formula; (height + width) ÷ 2. Growth was determined by the formula; final plant size index - initial plant size index. Plants were graded at termination of research based on a scale of 1 = dead, 2 = poor quality, unsalable, 3 = fair quality, salable, 4 = good quality and 5 = excellent quality.
In experiment 1, growing medium was amended at transplanting time with 1 lb/yd3 (0.59 kg/m3) Micromax (The Scotts Company, 6656 Grantway, Allentown, PA 18106) and 7.5 lb/yd3 (4.45 kg/m3) of one of the four dolomite products tested. This was a 4 fertilizer rate x 4 dolomite product factorial test with 5 replications per treatment. Starting on June 13, 1994, plants were fertilized once a week. Liquid fertilizer made from concentrated stock solutions was used, with NH4 and NO3 each providing 50% of the nitrogen source. When fertilized each pot received 100 ml fertilizer solution made up of NH4NO3, K2SO4 and H3PO4 so that fertilizer formulation was 6N-2P-5K. Fertilizer rates tested were 1222, 1833, 2444 or 3666 lb N/A/Yr, (1369, 2053, 2737 or 4106 kg/ha/yr) with 1833 lbs being the recommended level.
Electrical conductivity (µmhos/cm) and pH of the growing medium leachate were determined on June 9, July 7, August 9 and finally on September 7, 1994. Initial plant height and width (cm) were measured on June 8, 1994 and final height and width were determined on September 21, 1994. Plants were graded on September 26, 1994, when research was terminated.
In experiment 2, the four dolomite products were incorporated into the same basic growing medium as used in the previous experiment, each product at three different rates. For each product tested, Camille dieffenbachia were also grown using the basic potting mix without dolomite. There were 5 replications per treatment.
Fafard #4 growing medium, containing no lime, was amended with 1 lb/yd3 Micromax. Treatments consisted of each of the four dolomite products incorporated at 0.0, 2.5, 5.0, or 7.5 lb/yd3 (0.0, 1.48, 2.96 or 4.45 kg/m3 ). Plants were fertilized once a week using the same liquid feed as used for experiment 1, applied at the recommended rate of 1833 lb N/A/yr.
Electrical conductivity (µmhos/cm) and pH of the growing medium leachate was determined initially on June 9, 1994. Electrical conductivity and pH were then determined once a month throughout production, on July 6, August 8 and September 6, 1994.
Results
In experiment 1, interaction of dolomite source and fertilizer rate affected pH of growing medium leachate on July 7, August 9 and September 7, 1994 (Figures 1, 2 and 3). From July 7 until termination, growing medium leachate with higher pH, fertilized at any rate, were mainly those with incorporated James River Camadil or Asgrow dolomite, followed by James River and Soil Doctor, in order of decreasing pH. The first two products are made up of more finer particles compared to particle size makeup of Soil Doctor Dolomite and James River Dolomite (Table 1). On June 9, 1994, five days before fertilizer treatments were initiated, pH of leachate collected from growing medium of Camille dieffenbachia averaged 5.4. Over time, the increase in fertilizer rate from 2444 to 3666 lb/A/yr had a much greater acidifying effect on growing medium leachate compared to when rate was increased from 1222 to 1833 or from 1833 to 2444 lb/A/yr.
Although all plant grades were above 4.0 (good quality), plants grown in medium containing Asgrow or James River dolomite were slightly better than plants grown in medium containing James River Camadil dolomite or Soil Doctor dolomite (Table 2). particle size of these two products were more similar, when compared to particle size of the two other products tested (Table 1). Soil Doctor Dolomite had more larger size particles and James River Camadil had more smaller particles.
The recommended fertilizer rate of 1833, the second lowest rate, produced the largest best quality plants (Table 2). Plants grew less and received lower plant grades as fertilizer rate was increased above the 1833 lb/A/yr rate.
When pH was measured soon after incorporation, on June 9, growing medium leachate from products made up of finer dolomite particles had higher electrical conductivity compared to leachate collected from growing medium getting one of the two products having coarser particles (Table 3). On later sampling dates, however, electrical conductivity of the growing medium leachate was not significantly different due to dolomite source. Electrical conductivity of leachate from samples collected from July through September increased as fertilizer rate increased.
In experiment 2, when dolomite sources were compared, no significant differences due to dolomite source were found in plant grade, plant growth and electrical conductivity and pH of the growing medium leachate (data not shown). However, for each dolomite source tested, incorporation rate did affect pH and electrical conductivity of leachate and most plant growth measurements.
Electrical conductivity of leachate was variable in its response to increasing dolomite rate, although it generally increased (Tables 4 through 7). However, over time conductivity decreased, and this probably related to use of nutrients by the plants as well as leaching of calcium and magnesium from dolomite.
When the amounts of Asgrow dolomite in growing medium increased plant growth increased but plant quality was not similarly affected (Table 8). Increasing dolomite incorporation rate from 0 to 5.0 lb/yd3 produced a small but significant increase in plant growth and quality for Camille dieffenbachia getting any of the other three dolomite products (Tables 9 through 11). When the amount of any of these three products in the growing medium was increased from 5.0 to 7.5 lb/yd3 plants grew less compared to plants getting the 5.0 lb/yd3 rate and quality did not further improve.
Quality of all Camille dieffenbachia was better than good when the experiment was terminated, but increasing lime rate did slightly increase plant quality for two of the four products tested, Soil Doctor Dolomite and James River Camadil Dolomite. These two products were on opposite ends of the particle size scale (Table 1). (In experiment 1 use of either of these two products incorporated at 7.5 lb/yd3 the highest rate tested in experiment 2, produced slightly lower quality plants).
Conclusions
Results from experiment 1 reinforce the importance of following recommended fertilizer guidelines. Higher than needed fertilizer rates, regardless of dolomite product used, adversely affected plant quality, had a more acidifying effect on growing medium pH and produced an unnecessary increase leachate electrical conductivity.
Since plants require calcium and magnesium for healthy growth, it makes sense that potting mixes containing dolomite would produce larger, better quality plants compared to growing medium without a source of those two elements.
When incorporated at the rates used here, dolomite products having more particles in the moderate size range shown in Table 1 may be slightly better for Camille dieffenbachia production compared to dolomite products made up of more large or fine size particles. Even though the two products with finer particles did a slightly better job of raising the pH level, pH of growing medium incorporated with either of the two products having moderate size particles was well within the acceptable limits for healthy foliage plant growth, and produced slightly better quality plants than the growing media containing either of the two dolomite products made up of finer particle sizes.
These results also demonstrate that pH in itself is not an especially good indicator of the potential for production of quality foliage plants as long as a reasonable level of dolomite has been incorporated into the growing medium.
Fig. 1. Interaction of
dolomite source and fertilizer rate on pH of Ieachate collected
from growing medlum on July 7. 1994.
Interaction significant at P = 0.0001.
Fig. 2. Interaction of
dolomite souroe and fertilizer rate on pH of leachate collected
from growing medium on August 9, 1994.
Interaction significant at P = 0.0001.
References
Standard Sieve # |
Soil Particle size (µm) |
Soil Dr.z | James Rivery | Asgrowx | James River Camadily |
---|---|---|---|---|---|
+ 20 | > 850 µm | 16% | -- | -- | -- |
+ 50 | 300 to 850 µm | 19% | 5% | -- | -- |
+ 100 | 75 to 150 µm | 11% | 13% | -- | -- |
+ 200 | 75 to 150 µm | 10% | 30% | 6% | -- |
+ 325 | 45 to 75 µm | 12% | 19% | 20% | 5% |
- 325 | <45 µm | 32% | 33% | 74% | 95% |
Fig. 3. interaction of dolomite source and fertilizer rate on pH of leachate collected from growing medium on September 7, 1994.
Interaction significant at P = 0.0001.
Dolomite source | Growth indexx (cm) | Plant gradey |
---|---|---|
Asgrow | 30.4ax | 4.8a |
J. R. Camadil | 28.6b | 4.4b |
Soil Dr. | 29.9ab | 4.4b |
James River | 29.4ab | 4.7a |
Fertilizer ratew, lb N/A/Yr | ||
1222 | 28.8 | 4.5 |
1833 | 30.8 | 4.8 |
2444 | 30.2 | 4.6 |
3666 | 28.6 | 4.3 |
Significancev | ||
linear | ns | * |
quadratic | ** | ** |
Dolomite source | Jun.9 | Jul.7 | Aug.9 | Sep.7 |
---|---|---|---|---|
Asgrow | 2305ay | 2727a | 3953a | 1354a |
J.R. Camadil | 2228a | 2796a | 3366a | 1390a |
Soil Dr. | 1908b | 2823a | 3726a | 1695a |
James River | 2008b | 2651a | 3226a | 1300a |
Fertilizer rate, lb N/A/yr | ||||
1222 | 2095x | 1812 | 1510 | 297 |
1833 | 2090 | 2136 | 2963 | 679 |
2444 | 2226 | 2892 | 3962 | 1310 |
3666 | 2038 | 4158 | 5836 | 3452 |
Significancew | ||||
linear | ns | ** | ** | ** |
quadratic | ns | * | ns | ** |
Dolomite rate, lb/Yd3 | Jun 9 | Jul 6 | Aug 8 | Sep 6 |
---|---|---|---|---|
0.0 | 2112 | 1656 | 3086 | 1501 |
2.5 | 3308 | 2888 | 3446 | 1181 |
5.0 | 3260 | 3878 | 4716 | 1134 |
7.5 | 3592 | 3524 | 3722 | 759 |
Significancez | ||||
linear | ** | ** | ns | * |
quadratic | ** | ns | ns | ns |
Dolomite rate, lb/yd3 | Jun 9 | Jul 6 | Aug 8 | Sep 6 |
---|---|---|---|---|
0.0 | 3.3 | 3.9 | 3.0 | 2.8 |
2.5 | 4.0 | 4.4 | 3.4 | 3.3 |
5.0 | 5.1 | 5.0 | 4.6 | 4.8 |
7.5 | 5.2 | 5.3 | 5.1 | 5.2 |
Significancez | ||||
linear | ** | ** | ** | ** |
quadratic | ** | ** | ** | ** |
Dolomite rate, lb/Yd3 | Jun 9 | Jul 6 | Aug 8 | Sep 6 |
---|---|---|---|---|
0.0 | 1962 | 2846 | 3276 | 1600 |
2.5 | 3386 | 3042 | 3946 | 759 |
5.0 | 1664 | 2952 | 3220 | 830 |
7.5 | 2010 | 3092 | 4368 | 1146 |
Significancez | ||||
linear | ** | ns | ns | ns |
quadratic | ** | ns | ns | ** |
Dolomite rate, lb/yd3 | Jun 9 | Jul 6 | Aug 8 | Sep 6 |
---|---|---|---|---|
0.0 | 3.2 | 3.6 | 3.1 | 2.8 |
2.5 | 4.2 | 4.4 | 3.5 | 3.5 |
5.0 | 5.1 | 4.9 | 5.1 | 5.1 |
7.5 | 5.4 | 5.4 | 5.1 | 5.1 |
Significancez | ||||
linear | ** | ** | ** | ** |
quadratic | ** | ** | ** | ** |
zns, *, **; Nonsignificant, significant at P = 0.05 or significant at P = 0.01, respectively.
Dolomite rate, lb/Yd3 | Jun 9 | Jul 6 | Aug 8 | Sep 6 |
---|---|---|---|---|
0.0 | 1992 | 2760 | 3512 | 1334 |
2.5 | 2260 | 3028 | 3450 | 1326 |
5.0 | 2676 | 3168 | 3682 | 901 |
7.5 | 2498 | 3610 | 3356 | 1152 |
Significancez | ||||
linear | * | ** | ns | ns |
quadratic | ns | ns | ns | ns |
Dolomite rate, lb/yd3 | Jun 9 | Jul 6 | Aug 8 | Sep 6 |
---|---|---|---|---|
0.0 | 3.2 | 3.7 | 3.1 | 2.8 |
2.5 | 3.9 | 4.2 | 3.7 | 3.4 |
5.0 | 4.9 | 4.8 | 4.6 | 4.2 |
7.5 | 5.1 | 5.2 | 5.1 | 4.8 |
Significancez | ||||
linear | ** | ** | ** | ** |
quadratic | ** | ** | ** | ** |
zns, *, **; Nonsignificant, significant at P = 0.05 or significant at P = 0.01, respectively.
Dolomite rate, lb/Yd3 | Jun 9 | Jul 6 | Aug 8 | Sep 6 |
---|---|---|---|---|
0.0 | 1974 | 2898 | 3336 | 1148 |
2.5 | 2358 | 3152 | 3366 | 1139 |
5.0 | 3514 | 3362 | 4926 | 1836 |
7.5 | 3312 | 3698 | 4126 | 918 |
Significancez | ||||
linear | ** | * | ** | ns |
quadratic | ns | ns | ns | ns |
Dolomite rate, lb/yd3 | Jun 9 | Jul 6 | Aug 8 | Sep 6 |
---|---|---|---|---|
0.0 | 3.2 | 3.8 | 3.0 | 2.9 |
2.5 | 4.1 | 4.4 | 3.6 | 3.6 |
5.0 | 4.6 | 4.9 | 4.3 | 4.2 |
7.5 | 4.9 | 5.1 | 4.9 | 4.9 |
Significancez | ||||
linear | ** | ** | ** | ** |
quadratic | ** | ** | ** | ** |
Dolomite rate, lb/yd3 |
Final size indexz |
Growth indexy |
Plant gradex |
---|---|---|---|
0.0 | 41.2 | 27.8 | 4.6 |
2.5 | 42.0 | 28.2 | 4.7 |
5.0 | 43.5 | 29.9 | 4.8 |
7.5 | 43.8 | 30.0 | 4.9 |
Significancez | |||
linear | * | ** | ns |
quadratic | ns | ns | ns |
Dolomite rate, lb/yd3 |
Final size indexz |
Growth indexy |
Plant gradex |
---|---|---|---|
0.0 | 39.7 | 26.2 | 4.4 |
2.5 | 42.9 | 29.6 | 4.9 |
5.0 | 44.4 | 31.3 | 5.0 |
7.5 | 43.7 | 29.5 | 5.0 |
Significancew | |||
linear | ** | * | ** |
quadratic | ns | * | * |
Dolomite rate, lb/yd3 | Final size indexz | Growth indexy | Plant gradex |
---|---|---|---|
0.0 | 40.3 | 27.1 | 4.7 |
2.5 | 41.8 | 30.1 | 4.8 |
5.0 | 44.1 | 30.1 | 5.0 |
7.5 | 43.8 | 28.8 | 5.0 |
Significancew | |||
linear | ** | ns | * |
quadratic | ns | * | ns |
Dolomite rate, lb/yd3 | Final size indexz | Growth indexy | Plant gradex |
---|---|---|---|
0.0 | 41.8 | 27.9 | 4.7 |
2.5 | 43.7 | 30.8 | 4.9 |
5.0 | 43.6 | 30.1 | 4.9 |
7.5 | 42.3 | 27.7 | 4.9 |
Significancew | |||
linear | ns | ns | ns |
quadratic | ns | * | ns |