Potassium nutrition of irrigated potatoes in South Australia. I. Effect on tuber yield and the prediction of tuber yield response by soil analysis

1986 ◽  
Vol 26 (6) ◽  
pp. 717 ◽  
Author(s):  
NA Maier

Field experiments were conducted over 4 years at 25 sites throughout the main potato-growing areas of South Australia to calibrate the 0.5M sodium bicarbonate extraction procedure as a soil test for potassium and to examine the responses of irrigated potatoes to rates up to 1280 kg/ha K applied as potassium sulfate or potassium chloride either banded at planting or side-dressed after emergence. Potassium application at planting increased yield (P < 0.05) at 10 sites. The mean percentage yield deficit was 21%. There were significant correlations between relative yield and clay and sand contents, cation exchange capacity and bicarbonate-extractable potassium concentration in 0-15-cm surface soil samples collected before potassium fertiliser was applied. Percentage silt and pH were not correlated with relative yield. The bicarbonate-extractable potassium soil test accounted for 70% of the variance in relative yield compared with only 27% for percentage clay and 22% for cation exchange capacity. The prognostic critical bicarbonate-extractable potassium concentrations were: 153 -t 12 mg/kg for the Smith-Dolby bent hyperbola model, 143 mg/kg for the Cate-Nelson separation, and 133 or 176 mg/kg for the Mitscherlich model (concentrations at relative yields of 90 and 95% respectively). Yield responses are likely when soil bicarbonate- extractable potassium concentrations are below 120 mg/kg (deficient range), uncertain between 12 1 and 200 mg/kg (marginal range) and unlikely above 200 mg/kg (non-responsive range). Banding potassium chloride at planting significantly reduced yield compared with potassium sulfate at 2 out of the 14 sites used. The yield reductions occurred with potassium rates of 160 kg/ha or higher. There were significant increases in yield with side-dressing compared with basal application, at 2 of 5 responsive sites using rates of 320 kg/ha K or higher. None of the side-dressing treatments reduced tuber yields below control yields.


1986 ◽  
Vol 26 (6) ◽  
pp. 727 ◽  
Author(s):  
NA Maier

I compared the effects of potassium sulfate and potassium chloride fertiliser, at rates up to 1280 kg/ ha K, on the concentrations in petioles of the youngest fully expanded leaves and in harvested tubers of potassium, calcium (tubers only), magnesium, phosphorus, chloride and sulfur (petioles only) and on potassium: magnesium ratios in petioles. For the sites classified as deficient and marginal according to soil test potassium concentrations, increased application rates of potassium sulfate increased the potassium and sulfur concentrations and potassium: magnesium ratios in petioles and decreased magnesium, phosphorus and chloride concentrations. In tubers both potassium and magnesium concentrations increased as potassium sulfate rates increased, while calcium and phosphorus concentrations showed negative trends. Compared with potassium sulfate, potassium chloride resulted in higher potassium, calcium and chloride concentrations and lower sulfur concentrations. Chloride concentrations in petioles from many sites were much higher than those reported in other studies and were related to high chloride concentrations in irrigation waters. Significant correlations were obtained between bicarbonate- extractable potassium concentrations in the surface (0-1 5-cm) soils and potassium concentrations in petioles (r2 = 0.75***) and tubers (r2 = 0.84***). As bicarbonate-extractable potassium concentrations in the surface soils increased from 40 to 600 mg/kg, the potassium concentrations in tubers increased from 1.69 to 2.69% compared with an increase from 5.72 to 1376% in petioles. Significant correlations were obtained between relative yields ((mean treatment yields/maximum mean treatment yie1d)x 100) and potassium concentrations (dry weight basis) in petioles and tubers and potassium:magnesium ratios in petioles. The percentage of variance in relative yield accounted for by each regression was 67.9, 31.0 and 56.9% respectively. The potassium concentration in petioles was the most effective plant index to predict yield response to potassium. For petioles and tubers prognostic critical potassium concentrations of 11.30 k 0.26% and 2.19 � 0.11% respectively were established. Alternatively, a prognostic critical potassium:magnesium ratio of 14.8 � 0.8% was determined. The choice of the mathematical model used influenced the critical values obtained.



2006 ◽  
Vol 6 (1) ◽  
pp. 179-182 ◽  
Author(s):  
N. Abdu . ◽  
A.A. Yusuf . ◽  
A. Abdulkadir . ◽  
U.L. Arunah . ◽  
V.O. Chude . ◽  
...  


2017 ◽  
Vol 54 (5) ◽  
pp. 794-804
Author(s):  
BERNARD DUBOS ◽  
VICTOR BARON ◽  
XAVIER BONNEAU ◽  
ALBERT FLORI ◽  
JEAN OLLIVIER

SUMMARYPotassium chloride (KCl) is the most widely used fertilizer in oil palm (Elaeis guineensis) plantations and the rates applied are based on interpretation of leaf K contents. When no positive response on leaf K contents can be detected, no optimum content can be established whatever the yield response to KCl rates. We used data from 13 fertilization trials conducted on several continents to study the responses of leaf K, leaf Cl, leaf Ca and yield to KCl rates as a function of the soil properties of each site. We found that the abundance of exchangeable Ca in the soil expressed as a percent of the cation exchange capacity (CEC) was the best soil variable to predict if leaf K content would increase with KCl rates. In addition, we found that the leaf K contents of unfertilized controls at the end of the trials were also correlated with Ca/CEC. This ratio thus appears to be a better index of soil K reserves than soil exchangeable K content.



2018 ◽  
Vol 4 (1) ◽  
Author(s):  
Mardi Wibowo

Since year 1977 until 2005, PT. ANTAM has been exploited nickel ore resources at Gebe Island – Center ofHalmahera District – North Maluku Province. Mining activity, beside give economically advantages also causedegradation of environment quality espicially land quality. Therefore, it need evaluation activity for change ofland quality at Gebe Island after mining activity.From chemical rehabilitation aspect, post mining land and rehabilitation land indacate very lack and lackfertility (base saturated 45,87 – 99,6%; cation exchange capacity 9,43 – 12,43%; Organic Carbon 1,12 –2,31%). From availability of nutrirnt element aspect, post mining land and rehabilitation land indicate verylack and lack fertility (nitrogen 0,1 – 1,19%). Base on that data, it can be concluded that land reclamationactivity not yet achieve standart condition of chemical land.Key words : land quality, post mining lan





Author(s):  
Geraldo R. Zuba Junio ◽  
Regynaldo A. Sampaio ◽  
Altina L. Nascimento ◽  
Luiz A. Fernandes ◽  
Natália N. de Lima ◽  
...  

ABSTRACTThis study aimed to evaluate the chemical attributes of an Inceptisol cultivated with castor bean (Ricinus communis L.), variety ‘BRS Energia’, fertilized with sewage sludge compost and calcium (Ca) and magnesium (Mg) silicate. The experiment was conducted at the ICA/UFMG, in a randomized block design, using a 2 x 4 factorial scheme with three replicates, and the treatments consisted of two doses of Ca-Mg silicate (0 and 1 t ha-1) and four doses of sewage sludge compost (0, 23.81, 47.62 and 71.43 t ha-1, on dry basis). Soil organic matter (OM), pH, sum of bases (SB), effective cation exchange capacity (CEC(t)), total cation exchange capacity (CEC(T)), base saturation (V%) and potential acidity (H + Al) were evaluated. There were no significant interactions between doses of sewage sludge compost and doses of Ca-Mg silicate on soil attributes, and no effect of silicate fertilization on these attributes. However, fertilization with sewage sludge compost promoted reduction in pH and increase in H + Al, OM and CEC. The dose of 71.43 t ha-1 of sewage sludge compost promoted the best soil chemical conditions.



2005 ◽  
Vol 57 (3) ◽  
pp. 356-364 ◽  
Author(s):  
E. C. Bortoluzzi ◽  
D. Tessier ◽  
D. S. Rheinheimer ◽  
J. L. Julien


Materials ◽  
2021 ◽  
Vol 14 (10) ◽  
pp. 2617
Author(s):  
Alicja Szatanik-Kloc ◽  
Justyna Szerement ◽  
Agnieszka Adamczuk ◽  
Grzegorz Józefaciuk

Thousands of tons of zeolitic materials are used yearly as soil conditioners and components of slow-release fertilizers. A positive influence of application of zeolites on plant growth has been frequently observed. Because zeolites have extremely large cation exchange capacity, surface area, porosity and water holding capacity, a paradigm has aroused that increasing plant growth is caused by a long-lasting improvement of soil physicochemical properties by zeolites. In the first year of our field experiment performed on a poor soil with zeolite rates from 1 to 8 t/ha and N fertilization, an increase in spring wheat yield was observed. Any effect on soil cation exchange capacity (CEC), surface area (S), pH-dependent surface charge (Qv), mesoporosity, water holding capacity and plant available water (PAW) was noted. This positive effect of zeolite on plants could be due to extra nutrients supplied by the mineral (primarily potassium—1 ton of the studied zeolite contained around 15 kg of exchangeable potassium). In the second year of the experiment (NPK treatment on previously zeolitized soil), the zeolite presence did not impact plant yield. No long-term effect of the zeolite on plants was observed in the third year after soil zeolitization, when, as in the first year, only N fertilization was applied. That there were no significant changes in the above-mentioned physicochemical properties of the field soil after the addition of zeolite was most likely due to high dilution of the mineral in the soil (8 t/ha zeolite is only ~0.35% of the soil mass in the root zone). To determine how much zeolite is needed to improve soil physicochemical properties, much higher zeolite rates than those applied in the field were studied in the laboratory. The latter studies showed that CEC and S increased proportionally to the zeolite percentage in the soil. The Qv of the zeolite was lower than that of the soil, so a decrease in soil variable charge was observed due to zeolite addition. Surprisingly, a slight increase in PAW, even at the largest zeolite dose (from 9.5% for the control soil to 13% for a mixture of 40 g zeolite and 100 g soil), was observed. It resulted from small alterations of the soil macrostructure: although the input of small zeolite pores was seen in pore size distributions, the larger pores responsible for the storage of PAW were almost not affected by the zeolite addition.



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