EXCHANGEABLE AND WATER-SOLUBLE POTASSIUM IN SOILS AND DEGREE OF SATURATION IN RELATION TO TOMATO YIELDS

1959 ◽  
Vol 39 (2) ◽  
pp. 129-135 ◽  
Author(s):  
R. L. Halstead ◽  
H. B. Heeney
Keyword(s):  
Sandy Loam ◽  
Clay Content ◽  
Field Trials ◽  
Water Soluble ◽  
Degree Of Saturation ◽  
Yield Response ◽  
Clay Loam ◽  
Exchangeable Potassium ◽  
Potassium Fertilizer ◽  
Prince Edward County

In 33 field trials on soils varying in texture from sandy loam to clay loam in Prince Edward County, Ontario, exchangeable potassium, per cent potassium saturation, and water-soluble potassium were significantly correlated with yield response of tomatoes to potassium fertilizer on the sandy loam soils, but there was no correlation within the loam and clay loam groups. The mean c1 value in the modified Mitscherlich equation relating exchangeable potassium to yield response within the sandy loam group was 0.00555 and the coefficient of variation was 19.8 per cent. The corresponding coefficients for c1 values based on per cent potassium saturation and water-soluble potassium were of greater magnitude. The amounts of potassium soluble in boiling 1 N HNO3 were not related to yield response.Exchangeable potassium and the non-exchangeable form soluble in boiling 1 N HNO3 increased, whereas water-soluble potassium decreased with increasing clay content of the samples. Water-soluble potassium was significantly correlated with per cent potassium saturation within the sandy loam and loam groups.

RELEASE OF NON-EXCHANGEABLE SOIL POTASSIUM BY RESIN-EQUILIBRATION AND ITS SIGNIFICANCE FOR CROP GROWTH

1962 ◽  
Vol 42 (2) ◽  
pp. 266-272 ◽  
Author(s):  
T. E. Barber ◽  
B. C. Matthews
Keyword(s):  
Linear Regression ◽  
Ammonium Acetate ◽  
Cation Exchange Resin ◽  
Yield Response ◽  
Exchangeable Potassium ◽  
Quadratic Regression ◽  
Potassium Fertilizer ◽  
Crop Response ◽  
Soil Potassium ◽  
The Difference

The non-exchangeable potassium released by soil after equilibration with cation-exchange resin was determined by extraction of the mixture with neutral ammonium acetate at room temperature and compared with a similar extraction in the absence of resin. The difference obtained following a 2-day equilibration period was called moderately-available potassium.Simple linear regression of yield on exchangeable potassium or exchangeable plus moderately-available potassium accounted for only 16 and 27 per cent respectively of the variability in yield response of corn, wheat, oats and potatoes to potassium fertilizer in the field. Multiple linear regression of yield on exchangeable and moderately-available potassium accounted for an average of 37 per cent of the variation in crop response; but a multiple quadratic regression of Log (100-per cent yield) on exchangeable and moderately-available potassium accounted for an average of 56 per cent of the variability in Log (100-per cent yield). Multiple quadratic regression of absolute yield or per cent yield on exchangeable and moderately-available potassium accounted for 46 and 50 per cent, respectively, of the variability in crop response to potassium fertilizer.

Influence of Various Soil Properties on the Adsorption and Desorption of ICIA-0051 in Five Soils

1992 ◽  
Vol 6 (3) ◽  
pp. 583-586 ◽  
Author(s):  
John S. Wilson ◽  
Chester L. Foy
Keyword(s):  
Sandy Loam ◽  
Clay Content ◽  
Silty Clay ◽  
Silt Loam ◽  
Clay Loam ◽  
Soil Factors ◽  
Silty Clay Loam ◽  
Freundlich Equation ◽  
General Order ◽  
Highly Correlated

The soil organic matter and/or humic matter fraction was highly correlated with the adsorption of ICIA-0051 herbicide onto five soils; clay content and other soil factors were less correlated. The Freundlich equation was used to describe the adsorption of ICIA-0051 by the various soils. Based on the K constants, the general order for adsorption for each soil was Hyde silty clay loam > Frederick silt loam > Davidson clay = Bojac sandy loam > Appling loamy sand. Across all soils, 25 to 50% of the amount adsorbed was removed by two desorptions. Appling, Bojac, and Davidson soils retained less herbicide after two desorptions than did Frederick and Hyde.

The availability of potassium in some Tasmanian soils. I. The variability of soil potassium in the field and its fractionation

1960 ◽  
Vol 11 (5) ◽  
pp. 750
Author(s):  
AM Graley ◽  
KD Nicholls ◽  
CS Piper
Keyword(s):  
Nitric Acid ◽  
Hydrochloric Acid ◽  
Soil Type ◽  
Field Experiments ◽  
Sandy Loam ◽  
Water Soluble ◽  
Soluble Form ◽  
Exchangeable Potassium ◽  
Exchangeable Fraction ◽  
Total Potassium

The potassium status of Frodsley sandy loam and some associated soils from the Fingal district, north-eastern Tasmania, has been investigated. Regularly spaced sampling of surface soils on a rectilinear grid pattern disclosed a variability of exchangeable potassium values in the field much greater than recorded for soils elsewhere; even for 3-ft spacings there was a sevenfold range. The need for adequate sampling of experimental areas is stressed. The median value for exchangeable potassium in the A1 horizon of Frodsley sandy loam was 0.31 m-equiv./100 g for "developed" areas and 0.35 m-equiv./100 g for "undeveloped" areas. Values for the A2 horizon were closely correlated with those for the corresponding surface horizon, but only about one-third as high. The amounts in the B horizon tended to approximate to those in the A1 horizon except for soils with high values in the surface. The potassium-supplying capacity of the soils was assessed by fractionation of the potassium into water-soluble, exchangeable, difficultly exchangeable, hydrochloric acid-soluble, and total potassium. In Frodsley sandy loam approximately 35 per cent. of the exchangeable potassium appeared in the water-soluble form, which suggested that there may be moderate losses from this soil by leaching. Ten minutes' boiling with normal nitric acid released only about 90 per cent. more potassium than was present in the exchangeable fraction. Boiling normal nitric acid extracted much less potassium from some samples of this soil type than did cold normal ammonium chloride from others, because of the great variability of exchangeable potassium. Concentrated hydrochloric acid dissolved a further 0.60.7 m-equiv./100 g on the average. These low values for the two latter fractions are taken to indicate the poverty of this soil type in reserves of potassium and, with the relatively low values for the exchangeable fraction, explain the widespread responses to potassium reported in field experiments. Examination of the minerals of the clay fraction of Frodsley sandy loam supported the chemical data in regard to the poor potassium status of these soils. Separation of sand, silt, and clay from the B horizons of two profiles showed that much of the total potassium was present in the coarser fractions of the soil. Type A, a soil associated with Frodsley sandy loam on river terraces, had a similar potassium status. Soils formed on dolerite were significantly higher in all categories of potassium.

Root Growth and Yield Response of Rainfed Lowland Rice to Planting Method

1987 ◽  
Vol 23 (3) ◽  
pp. 305-313 ◽  
Author(s):  
P. K. Sharma ◽  
S. K. De Datta ◽  
C. A. Redulla
Keyword(s):  
Root Growth ◽  
Grain Yield ◽  
Water Table ◽  
Sandy Loam ◽  
Lowland Rice ◽  
Yield Response ◽  
Clay Loam ◽  
Transplanted Rice ◽  
Rainfed Lowland ◽  
Loam Soil

SUMMARYField experiments were conducted on two soils (clay loam and sandy loam) with varying texture and water table depth to study the effects of two planting methods (dry seeding and transplanting) on the root growth and grain yield of rainfed lowland rice. About 75% of the roots were found in the top 10 cm soil. Root length density at the flowering stage and grain yield in the sandy loam soil, with a water table deeper than 1.5 m, were less in dry-seeded than in transplanted rice, probably because of the greater moisture stress in dry-seeded rice between late tillering and harvest. In the clay loam soil, with the water table mostly at the soil surface, there was no difference in grain yield between dry-seeded and transplanted rice.

Sodium and Potassium Fertilizer in Relation to Soil Physical Properties and sugar-beet yield

1976 ◽  
Vol 87 (3) ◽  
pp. 633-642 ◽  
Author(s):  
A. P. Draycott ◽  
M. J. Durrant ◽  
D. B. Davies ◽  
L. V. Vaidyanathan
Keyword(s):  
Sugar Beet ◽  
Physical Properties ◽  
Soil Structure ◽  
Field Experiments ◽  
Sandy Loam ◽  
Seedling Emergence ◽  
Fine Sand ◽  
Clay Loam ◽  
Potassium Fertilizer ◽  
Visual Assessments

SummaryDespite much experimental evidence showing that sodium fertilizer increases sugar–beet yield and decreases need for potassium, there is resistance to its use on some soil types through fears of deterioration in soil structure. Twelve field experiments with sugar beet were made in Eastern England, testing all combinations of autumn and spring applications of 0, 150 and 300 kg Na/ha and 0, 83 and 333 kg K/ha. Fields were chosen with soils of loamy very fine sand, very fine sandy loam, sandy clay loam and clay loam textures. Micro–plot and controlled environment studies were also made with the same soils to examine effects of sodium on seedling emergence and growth.Visual assessments of soil physical state following sodium application revealed no effect in the year sugar beet was grown nor in the following spring when cereals were grown. Measurements of physical properties of soils treated with sodium suggested that applications of several times the recommended amounts of sodium fertilizer would not damage soil structure. However, sodium fertilizer increased the osmotic suction of soil solution which, under some circumstances, e.g. dry springs or giving the fertilizer close to the time of sowing, decreased germination and seedling growth. For this reason and not because it has a detrimental effect on soil physical condition, sodium fertilizer best given in the autumn or some weeks before sowing.

The availability of potassium in some Tasmanian soils. II. Exhaustive cropping in relation to potassium reserves in the soil

1960 ◽  
Vol 11 (5) ◽  
pp. 774 ◽  
Author(s):  
CS Piper ◽  
Vries MPC de
Keyword(s):  
Sandy Loam ◽  
South Australia ◽  
Subterranean Clover ◽  
Yield Response ◽  
Exchangeable Potassium ◽  
Severe Deficiency ◽  
Intensively Managed ◽  
High Level ◽  
Yield Responses ◽  
Severe Leaf

Five soil samples from Fingal, Tas., representing Frodsley sandy loam of varying exchangeable potassium status, were subjected to exhaustive cropping in pots and the changes in their potassium status and that of the crops measured. Three of the samples represented an area carrying improved pastures while two were from a less intensively managed property. The results were contrasted with those from two soils from South Australia (Urrbrae loam and Seddon gravelly sandy loam). The progressive removal of potassium by cropping was determined by analysis of each crop and of the soil at the end of the experiment. Uptake and removal of potassium was greatest from the soils of highest exchangeable potassium status. Potassium applied to the soils was also rapidly taken up by the crops. For the Tasmanian soils, applications of potassium gave no responses in yield until the level of exchangeable potassium in the control pots fell to 0.10-0.15 m-equiv./100 g. The higher the initial level of exchangeable potassium, the greater the number of crops before a yield response to applied potassium was obtained. In contrast, yields were maintained at a high level on Urrbrae loam and, even in the fourth crop, applications of potassium gave only a barely significant response. From Frodsley and Seddon soils only small amounts of potassium were taken up from non-exchangeable sources. From Urrbrae loam, in the absence of applied potassium, slightly more than half of the potassium taken up by the crops was derived from other than exchangeable sources. These differences were in keeping with the different amounts of potassium released to boiling nitric acid by these soils. After four crops exchangeable potassium was reduced to very low levels (0.05-0.14 m-equiv./100 g) in all five Tasmanian soils. These values were directly related to the amounts of difficultly exchangeable potassium in these soils. Exchangeable potassium in Urrbrae loam was not reduced below 0.33 m-equiv./100 g, again reflecting the higher reserve of difficultly exchangeable potassium in the illitic clay of this soil and its greater capacity to replenish the exchangeable potassium fraction. The percentage of potassium in the dry matter of the crop was closely related to the level of exchangeable potassium or exchangeable plus added potassium in the soil. Subterranean clover showing severe leaf necrosis due to potassium deficiency contained 0.55-0.63 per cent. potassium. Plants showing less severe deficiency symptoms or symptoms developing at a later stage showed 0.84-0.98 per cent. potassium. Plants with 1.20 per cent. potassium were free from symptoms and gave no further yield responses to applied potassium. Additions of potassium to the soil led to higher values in the plants, and luxury uptake was common. At least 84-95 per cent. of the applied potassium was taken up by the crops on four of the Tasmanian soils.

Evaluation of Cotton Responses to Fomesafen-Based Treatments Applied Preemergence

2018 ◽  
Vol 32 (4) ◽  
pp. 431-438 ◽  
Author(s):  
Xiao Li ◽  
Timothy Grey ◽  
William Vencill ◽  
James Freeman ◽  
Katilyn Price ◽  
...  
Keyword(s):  
Field Experiments ◽  
Yield Loss ◽  
Sandy Loam ◽  
Clay Content ◽  
Dry Weight ◽  
High Rate ◽  
Growth And Yield ◽  
Effective Control ◽  
Yield Response ◽  
Cotton Yield

AbstractFomesafen provides effective control of glyphosate-resistant Palmer amaranth in cotton. However, cotton seedlings can be injured when fomesafen is applied PRE. Therefore, greenhouse and field experiments were conducted at Athens, GA, and at six locations in Alabama and Georgia in 2013 and 2016 to evaluate cotton growth and yield response to fomesafen applied PRE at 70, 140, 280, 560, 1,120, or 2,240 g ai ha−1, and in combination with pendimethalin, diuron, acetochlor, and fluridone at 1×label rates. Greenhouse bioassays indicated that fomesafen reduced cotton height and dry weight with increasing rate in Cecil sandy loam and Tifton loamy sand but not in Greenville sandy clay loam––possibly as a result of this soil’s higher organic matter (OM) and clay content. Fomesafen applied at 2,240 g ai ha−1 reduced cotton stand by as much as 83% compared to the nontreated check (NTC) at all field locations except Alabama’s Macon and Baldwin counties, and 1,120 g ai ha−1 reduced cotton stand only at Pulaski County, GA, by 52%. Cotton height was reduced by the two highest rates of fomesafen at all locations except Clarke County, GA, and Baldwin County, AL. Injury data indicated more visual injury followed increasing fomesafen rates, and high-rate treatments produced more injury in sandier soils. Cotton yield was unaffected by herbicide treatments at any location, except for the 1,120 g ai ha−1 rate at Pulaski County (49% yield loss compared to NTC), 2,240 g ai ha−1 at Pulaski County (72% yield loss), and Tift County (29% yield loss). These data indicated cotton yield should not be negatively affected by fomesafen applied PRE alone within label rates or in combination with pendimethalin, diuron, acetochlor, and fluridone at 1×label rates, although some visual injury, or stand or height reduction may occur early in the growing season.

Effect of potassium fertilization of pyrethrum (Tanacetum cinerariifolium) on yield, pyrethrins concentration in dry achenes and potassium concentration in soil and plant tissues

1994 ◽  
Vol 45 (3) ◽  
pp. 647 ◽  
Author(s):  
AA Salardini ◽  
KSR Chapman ◽  
RJ Holloway
Keyword(s):  
Field Experiments ◽  
Sandy Loam ◽  
Northern Region ◽  
Control Treatment ◽  
Yield Response ◽  
First Year ◽  
Clay Loam ◽  
Maximum Increase ◽  
Tanacetum Cinerariifolium ◽  
Second Year

Pyrethrum (Tanacetum cinerariifolium), a small perennial plant, has been commercially grown for production of pyrethrins (Py) in Tasmania since 1983. Two field experiments were conducted on clay loam and sandy clay loam krasnozem soils at Harford and North Motton in the northern region and a two-year experiment on an alluvial sandy loam at Ouse in the southern region of Tasmania to study its potassium (K) requirements. Potassium, at rates up to 200 kg K ha-1, was band-placed at planting (basal K) of pyrethrum splits. At Ouse in the spring of the following year up to 100 kg K ha-1 was side-dressed in the subplots. No achene yield response was observed at Harford with the soil Colwell K (Kc) of 80 mg K kg-1 and North Motton (Kc = 132), but at Ouse (Kc = 50) in the first year a maximum increase of 86% in the achene yield was attained at 50 kg K ha-1. In the second year at Ouse, the achene yield response occurred with residual basal K up to the 200 kg ha-1 rate, where the achene yield was 3.9-fold greater than the control. In addition to the increase gained from the residual K in the second year, 50 kg side-dressed K ha-1 increased the achene yield by a maximum of 50%. Basal K did not have any effect on the Py concentration of the first year crops, but it increased the Py concentration in the second year crop at Ouse. Side-dressed K also increased the Py concentration. The Py yield at the highest rate of 200 kg basal and 25 kg side-dressed K ha-1 was more than 6.5-fold that in the control treatment. The Kc and the concentration of K in apical tissues were correlated to the rates of applied K, achene yield and Py yield, and their potential as techniques to predict pyrethrum response to K application is discussed.

The movement of potassium in irrigated and fertilized red sandy clay

1940 ◽  
Vol 30 (3) ◽  
pp. 499-502 ◽  
Author(s):  
D. Lachower
Keyword(s):  
Irrigation Water ◽  
Soil Profile ◽  
Fertilizer Application ◽  
Water Soluble ◽  
Exchangeable Potassium ◽  
Potassium Fertilizer ◽  
Soil Potassium ◽  
Sandy Clay

The present investigation was intended to furnish information concerning:(1) The movement of water-soluble and exchangeable potassium in the soil profile after successive fertilizer applications.(2) The form of potassium—exchangeable, soluble, or non-exchangeable—into which added potassium fertilizer is converted in the soil.(3) The effect of doubling the fertilizer ration on the absorption of potassium by the soil; and the effect of doubling the ration of irrigation water on the absorption and accumulation of potassium in the soil.(4) The effect of frequent successive summer irrigation following fertilizer application on the distribution of the three forms of soil potassium.(5) The effect of fertilization followed by irrigation on soil pH. value.

Effect of fertilizer placement on yield of established alfalfa stands

1995 ◽  
Vol 75 (4) ◽  
pp. 883-887 ◽  
Author(s):  
R. G. Simons ◽  
C. A. Grant ◽  
L. D. Bailey
Keyword(s):  
Sandy Loam ◽  
Fertilizer Application ◽  
Forage Yield ◽  
Yield Response ◽  
Clay Loam ◽  
Clay Loam Soil ◽  
Fine Sandy Loam ◽  
Loam Soil ◽  
Four Levels ◽  
K Fertilization

Alfalfa yield response to P and K fertilization management has been documented elsewhere, but little work has been done in western Canada. Field studies conducted on two Manitoba soils for 4 yr evaluated the effects of four levels of monoammonium phosphate and three levels of potassium chloride fertilizers, applied as a surface broadcast or as an in-soil band application, on the yield of established alfalfa (Medicago sativa L.) stands. Applied P increased total annual forage yield on the clay loam soil by 1.53 t h−1 (47%), when averaged over the 4 yr of the study, but did not increase yields on the fine sandy loam. Yield response to P application on the clay loam soil increased over the 4 yr of the study. Potassium application resulted in minor or no increases in forage yield on both soils. On the clay loam soil, there was no yield difference between banded and broadcast fertilizer applications. On the fine sandy loam soil, band application reduced yields slightly compared with broadcast application, particularly at the first harvest following fertilizer application. Grass ingress into the plots was reduced by K application but was not affected by P fertilization, which may indicate a beneficial effect of K fertilization on alfalfa vigor and persistence. Key words: Potassium, phosphorus, banding, broadcast, persistence

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