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1.
Abstract

The main objective of this study was to determine the efficacy of cement kiln flue dust as a substitute for potassium sulfate fertilizer. Chemical and X‐ray diffraction analyses revealed that the flue dust contained about 20.7% K of which 9.1% was present as aphthitalite (K3Na(SO4)2) , 4.4% as sylvite (KCl) and the remaining 7.2% as arcanite (K2SO4) . Accordingly, about 80% of the potassium in the dust was present as sulfates, though it contained 30% total sulfate and 15% Ca.

The effects of flue dust were compared to some or all of the following fertilizers: KCl, K2SO4 and a synthetic fertilizer, on 11 soils ranging in texture from sand to clay in three greenhouse experiments. The synthetic fertilizer was made from K2SO4 and CaSO4.2H2O which were applied at the same rate of K and Ca as contained in the flue dust. The experimental results show that flue dust is as effective a K source as any of the fertilizers tested as it increased potato, barley and alfalfa yields and tissue and soil K concentrations to the same level. Furthermore, the flue dust increased the tissue sulfur concentration and the quantities of available sulfate in soils to the same level as potassium sulfate. Finally, the Ca contained in flue dust increased the concentration of this element in potato tops and soils when grown on eight coarse textured soils. The flue dust had, however, no effect on soil pH on any of the soils tested.  相似文献   

2.
Relative effectiveness of various hardly soluble K materials as sources of slow availability for plants was compared by uptake of K in Brassica seedlings grown in quartz sand-nutrient medium with occasional leaching, and by the release pattern of K.

Material characteristics exert a great influence on K availability. Water solubility is not a dominant factor for controlling the availability of K to the plants, but particle sizes and the reaction of K in fertilizers with nutrient ions in the medium play a significant role in the release pattern of K. Moreover, the plant roots have an ability to accelerate K release from such hardly soluble aources as fused potassium phosphate, KMgPO4, and K2CaP2O7.

According to the results obtained, that is, total dry matter production, pattern of K uptake through four successive croppings and loss of K by leaching the examined materials appear to be divided into the following three groups:

  • a) Materials having a high degree of slow availability-KMgPO4 (+3 mesh), fused potassium phosphate (+28 mesh and -65 mesh), K2CaP2O7 (+3 mesh), and calcined potassium phosphate (-7+14 mesh).

  • b) Materials having a mid degree of slow availability- KCaPO4 (+3 mesh), liparite potassium. Sulphur coated KCl, calcined potassium phosphate (-32 mesh), K2CaP2O7 (-32 mesh), KMgPO4 (-32 mesh), and KPO3 (+3 mesh).

  • c) Materials having a low degree of slow availability-KCaPO, ( -32 mesh), KPO, (-32 mesh).

  相似文献   

3.
Abstract

To evaluate the relationship between the amount of available Silicon (Si) in paddy soils and their mineral properties on the Shounai Plain in Japan, which is formed from several parent materials, we evaluated the amount of available Si, the particle size distribution, the oxide composition of crystalline minerals and the amount of oxalate-extractable Si (Sio), iron (Feo) and aluminum (Alo) in the soil. The amount of available Si in the soil and the oxide content of the crystalline minerals differed among four soil groups that were distinguished by their clay mineral composition. There was no difference in the particle size distribution among the soil groups. The amount of available Si was positively related to the SiO2/Al2O3 ratio of clay, the CaO concentration of silt and fine sand, and the amounts of Sio, Feo and Alo in the soil. The amount of available Si in the soils was negative correlated with the Na2O and K2O concentrations of silt, the K2O concentration of fine sand, and the coarse sand content. These results suggest that the amount of available Si in soils is affected by the weathering resistivity of their minerals and that the particle size distribution and mineral composition are related to the available Si of the soils. Mineralogical properties, including the particle size distribution and mineral composition such as the SiO2/Al2O3 ratio × clay fraction content and the amounts of CaO and MgO in silt-sized particles, were positively correlated with the amount of available Si in the soil, but these correlations were not found for fine sand-sized particles. The Sio, Feo and SiO2/Al2O3 ratio × clay fraction contents contributed approximately 50% to the amount of available Si in the soils. The amount of available Si in the soil was divided into two groups according to the location of the paddy field. The amount of soil-available Si in the alluvial plain was affected by the geology upstream through the mineral composition.  相似文献   

4.
Abstract

Calcium lignosulphonate (CaLS), a waste product from the pulp and paper industry, is expected to affect reaction of K fertilizer in the soil, thus influences their availability to crops. A clay soil (Typic Humaquept) was incubated with various amounts of CaLS (0 to 150 g kg‐1 soil) and potassium dihydrogen phosphate (0–25.64 mmol kg‐1 soil) for 240 h under moist conditions at 5 and 15°C. Subsamples were extracted with deionized water and the Mehlich‐III (M3) solution for the analyses of pH, and P, Ca, K and Mg concentrations and K adsorption (Kad). Higher temperature reduced M3 extractable K (KM3). CaLS and K additions increased M3 extractable Mg (MgM3) with Ca contributed more than did K as indicated by the standardized estimates. Additions of CaLS increased KM3. Potassium adsorption decreased with the increases in CaLS addition rates. Significant positive linear relationships were observed between Kad and the concentration ratio of [K+]/[Ca2+]½, suggesting that the potassium buffering capacity of the soil was reduced by the additions of CaLS, with the desugared CaLS being more effective than the non‐desugared CaLS. The increased slope values with the increases in CaLS additions of the linear relationships between KM3 and [K]/[Ca2+]½ indicated that CaLS improved the quantity and intensity relationships and increased the power of the soil supplying plants with K.  相似文献   

5.
不同施肥方法对双季稻区水稻产量及氮素流失的影响   总被引：8，自引：2，他引：8  
为保障粮食安全,减少稻田生态系统氮肥投入,提高氮肥利用率和减少氮素流失成为重要的农业和环境措施。本研究在位于湖南岳阳的农业部岳阳农业环境科学观测实验站开展为期1年的早稻、晚稻田间试验,比较了不施肥(T_1)、尿素常规施肥(T_2,施N 280 kg·hm~(-2)、P_2O_5 165 kg·hm~(-2)、K_2O 120 kg·hm~(-2))、控释肥常规施用(T_3,施N 230 kg·hm~(-2)、P_2O_5 165 kg·hm~(-2)、K_2O 120 kg·hm~(-2))、高量控释肥侧条施用(T_4,施N 230 kg·hm~(-2)、P_2O_5 138 kg·hm~(-2)、K_2O 120 kg·hm~(-2))、中量控释肥侧条施用(T5,施N 180 kg·hm~(-2)、P_2O_5 123 kg·hm~(-2)、K_2O 120kg·hm~(-2))及低量控释肥侧条施用(T6,施N 140 kg·hm~(-2)、P_2O_5 123 kg·hm~(-2)、K_2O 120 kg·hm~(-2))下氮肥的养分利用率、作物产量及氮素流失情况,以期为稻田氮素合理利用提供理论依据。研究结果表明,控释肥侧条施用可有效提高水稻的产量和氮肥利用率,减少面源流失。1)在减少稻田秧苗数量和氮肥施用量的条件下,T_4处理的水稻早晚稻产量分别比T_2处理增加13.17%和4.72%,与T_3处理相比亦分别增加7.27%和1.74%;2)侧条施肥处理有效降低了稻田氮素流失量,年氮流失量为0.466~0.673 kg×hm~(-2),比常规施肥处理降低地表径流氮流失量3.54%~29.36%;3)侧条施肥有效提高了氮肥利用率,T_4处理的氮肥利用率分别是T_2、T_3处理的1.70倍和1.22倍。因此,采用合适的施肥方式、配施适量控释氮肥可获得较高的产值和收益。高量控释肥侧条施用(T_4)是本研究区域最佳的施肥模式,对实现现代化农业生产的高产高效、资源节约和生态环境保护具有重要意义。  相似文献   

6.
通过5年定位试验（2008~2012年）, 研究不同钾肥施用量对水稻产量、植株钾素含量、钾素积累量、钾肥利用率、土壤钾素含量、钾素平衡和钾肥经济效益的影响。试验施钾量（K2O）从低到高设K0（不施钾）、K1（早稻84 kg/hm2、晚稻105 kg/hm2）、K2（早稻120kg/hm2、晚稻 150 kg/hm2）、K3（早稻156kg/hm2、晚稻195 kg/hm2）和K4（早稻192kg/hm2、晚稻 240kg/hm2）5个处理。5年的试验结果表明, 施钾能显著提高早、晚稻产量,在一定施钾量范围内,水稻产量随施钾量的增加而增加;施钾能促进水稻植株对钾素的吸收和积累,尤其是稻草对钾素的吸收和积累;早、晚稻的钾肥农学效应均以K2处理最高（早稻3.12 kg/kg、晚稻3.70 kg/kg）;钾肥利用率以K1处理最高（早稻41.2%、晚稻76.4%）,并随施钾量提高而降低;不同施钾量对土壤钾素含量有明显影响,土壤速效钾、缓效钾和土壤全钾均随施钾量的增加而增加,且不同处理间土壤速效钾含量差异达极显著水平（P＜0.01）;连续种植5年10季水稻后,K0、K1和K2处理的土壤钾素亏缺（K 127.1kg/hm2、 58.3kg/hm2和10.8kg/hm2）,亏缺量随施钾量的增加而降低; K3和K4处理的土壤钾素盈余（48.0 kg/hm2 和109.2kg/hm2）,盈余量随施钾量的增加而增加。在经济效益上,早、晚稻产投比均以K2处理最高（早稻1.04、晚稻1.27）。综合考虑施钾的增产效应、经济效益和土壤钾素养分平衡等因素,建议该双季稻区早稻施钾量在K2O 120~156 kg/hm2、晚稻施钾量在K2O 150~195kg/hm2范围内较为适宜。  相似文献   

7.
K-struvite (potassium magnesium phosphate, KMgPO4.6H2O) is a promising multinutrient slow-release fertilizer; however, it may contain cadmium (Cd) in significant ranges like other phosphorus (P) fertilizers. This paper focuses on dissolution of a synthesized K-struvite in water, acid solutions and complexing agents. Firstly, K-struvite was synthesized by using Cd containing phosphoric acid (H3PO4). After its characterization, a three-stage dissolution study was carried out. The release of nutrient elements and Cd into extracts was studied. Phosphorus (P) and potassium (K) solubilities in pure water are low, not more than about 2.5% at the end of three extractions. It was found that solubility increased with the presence of mineral and organic acids. The presence of complexing agents also enhanced the dissolution of K-struvite. At the end of three extractions, citric acid (CA, C6H8O7.H2O) solution solubilized P about 38%, while dissolved K was about 35%, in cumulative. In the case of 0.001 mol/L Na2EDTA (C10H14N2Na2O8.2H2O), the solubilized K-struvite was found to be about 40%, which was about 14% in a 250 mg/L Na-humate. The maximum concentrations of Cd in the third extracts of hydrochloric acid (HCl), CA, oxalic acid (OA, C2H2O4) and Na2EDTA were measured to be in the range of about 14–19 μg/L, which corresponds to a Cd solubilization more than 46% for the three successive extractions.  相似文献   

8.
In order to establish critical potassium (K) concentration levels and K/calcium (Ca) plus magnesium (Mg) [K/Ca+Mg] ratios in potato petioles associated to maximum total tuber yields, an experiment was conducted under Brazilian conditions. Six K levels (0, 60, 120, 240, 480, and 960 kg K2O/ha as potassium sulphate) were applied in a randomized complete block design experiment with four replications. Baraka potato tubers were seeded, spaced 0.8 x 0.3 m, following the agronomic cultural practices recommended for the crop. After 48 days from plant emergence, plant tissue samples was collected from each plant, the youngest fully expanded leaves (YFEL) and the oldest but not senescent leaves (ONSL). Petioles from these leaves were analysed to their K, Ca, and Mg contents. At harvest, total, high grade, and weight tuber yields were increased to 733, 719, and 660 g/plant for the 353, 335, and 384 kg K2O/ha levels, respectively. These yields are double the Brazilian potato yield average. Petiole Ca and Mg concentrations were decreased by the K fertilizer treatments, whereas the opposite occurred with the K/Ca+Mg ratio. Potassium concentrations in the petioles from the YFEL and ONSL increased up to 10.44 and 7.13 g K/100 g petiole dry matter at the 672 and 654 kg K2O/ha levels, respectively. The K petiole gradient concentration was not affected by K fertilization. The K/Ca+Mg ratio for YFEL associated with the maximum total tuber yield was 7.24, while the K concentrations were 8.91 and 6.16 g K/100 g dry matter in petioles for the YFEL and ONSL, respectively.  相似文献   

9.
Gladiolus corms were grown in media contaminated with cadmium (Cd) (50 mg kg?1) and supplemented with silicon (Si) and potassium (K). The role of Si and K for mitigation of Cd toxicity was evaluated. Cd-induced stress generated significantly increased level of oxidative stress markers including hydrogen peroxide (H2O2), and malondialdehyde (MDA) in gladiolus. The application of K and Si improved the production of protein and proline in the treated plants. Moreover, K and Si supplemented plants exhibited an improvement in the activity of antioxidant enzymes and a reduction in the level of MDA, H2O2 and Cd uptake under Cd stress. Application of K and Si also enhanced the uptake of mineral nutrients including calcium (Ca), magnesium (Mg), manganese (Mn), sulfur (S) and K. The plants supplemented with K and Si exhibited a higher amount of total phenolics and flavonoids. The combined effect of Si and K was more pronounced regarding beneficial effects on gladiolus plants compared to individual effect of these elements under Cd stress. The current research reveals that Si and K may improve gladiolus growth by decreasing the oxidative stress and Cd uptake and by increasing the activity of antioxidant defense enzymes, the quantity of secondary metabolites and plant nutrition.  相似文献   

10.
ABSTRACT

The response of ‘Kurdistan’ and ‘Paros’ strawberry cultivars to potassium silicate (K2O3Si) under sodium chloride (NaCl) salinity stress was studied in terms of vegetative parameters, sodium (Na) and potassium (K) content and fruit quality. K2O3Si could recover dry mass distribution of NaCl-stressed strawberry organs. Kurdistan cultivar tended to keep higher dry weight of leaves to maintain its photosynthetic apparatus activity. Inhibitory impact of K2O3Si on Na uptake of leaf was more obvious than root. Implementation of K2O3Si in some cases increased Total Soluble Solid (TSS) and Titratable Acidity (TA), which are the main factors determining taste of strawberry fruit. Furthermore, phenols and flavonoids were increased in Paros cultivar by effect K2O3Si under saline and non-saline conditions, respectively. Overall, our data suggest that silicon supply in strawberry plants not only could be used as a routine strategy to maintain growth and yield under salinity but also it could be beneficial for improvement of fruit quality attributes and health-related constituents.

Abbreviations: ANOVA: Analysis of Variance; CRD: Completely Randomized Design; DPPH: 1,1-Diphenyl-2-picryl-hydrazyl; FF: Fruit Firmness; LSD: Least Significant Difference; PAL: Phenyl Alanine Ammonia Lyase; ROS: Reactive Oxygen Species; TSS: Total Soluble Solid; TAA: Total Antioxidant Activity; TA: Titratable Acidity; TAC: Total Anthocyanin; TF: Total Flavonoids; TP: Total Phenolics;  相似文献   

11.
磷、钾营养对套作大豆钾素积累及利用效率的影响   总被引：4，自引：0，他引：4  
以贡选1号为材料,研究了磷、钾营养对套作大豆钾素积累及利用效率的影响。结果表明,套作大豆全生育期钾素积累动态符合"S"型增长曲线。完熟期钾素积累总量以及根、茎、叶片、荚果各器官钾素含量均随施钾量增加而增加,随施磷量增加呈先增加后减少的趋势;各处理均以P2K3(P2O517.0 kg/hm2,K2O 112.5 kg/hm2)最高,较不施磷、钾(P0K0)高18.79%5~8.33%。全生育期钾积累速率呈单峰曲线变化,随施钾量增加而增加,随施磷量增加先升高后降低,出苗后90 d左右达到最大值。钾素生产效率、吸收利用率、农学利用率随施磷、施钾量增加与钾积累速率表现一致,但收获指数随施磷量增加先降低后升高。合理施用磷、钾肥能提高套作大豆钾素利用效率,以P2K1(P2O517.0 kg/hm2,K2O 37.5 kg/hm2)处理最好。  相似文献   

12.
Three K silicates having SiO2/K2O ratios of 4, 5, and 6 were compared with single and split applications of KCI, (KPO3)n, and sulfur-coated KCI (SCK-34) for their availability to four cuttings of common bermudagrass. At the rate of 200 mg of K/pot, all silicates applied in fine particles gave the same pattern of yield and K uptake as readily soluble KCl; however, less response to these finely sized K silicates at applications from 200 to 500 mg of K/pot suggests that they supply K more slowly than do soluble sources. K2O.6SiO2, when granulated in the size of 0.41-1.2 or 1.65-2.36 rom gave typical yieiJ and K uptake patterns of slowrelease sources similar to those for SCK-34 at both rates of application. (KPO3) n supplied K in the same pattern as KCl and no effect of granulation was observed. A better balanced K supply through the whole period and the production of forage of more stable mineral composition is expected by the use of these slow-release K sources.  相似文献   

13.
 The release of SO4 2–-S, K+, Ca2+ and Mg2+ from soil amended with spent mushroom compost (SMC), a byproduct of mushroom production, was measured in leachate from field lysimeters for 30 weeks. Rates of application were 0 and 80 t ha–1 moist SMC. The SMC contained 1.7% K, 6.5% Ca, 0.4% Mg and 1.2% S (of which 87% is SO4 2–-S), and has a C : S ratio of 26. The break-through curves of ion leaching were polymodal indicating the preservation of soil structure in the lysimeters and its influence on leaching. SO4 2–-S release from SMC was rapid (first-order exponential) and was very similar to the release from a laboratory incubation. The release of K+, Ca2+ and Mg2+ was described using first/zero-order models which were also used to describe their release in the laboratory. The rate and amount of Ca2+ release was similar in the field and laboratory, but the amount of K+ (and to a lesser extent Mg2+) release was less in the field than in the laboratory. Recoveries of SMC applied nutrients in leachate were 80% of S (263 kg ha–1), 3% of K (14 kg ha–1), 16% of Ca (284 kg ha–1) and 37% of Mg (40 kg ha–1). Little if any S was mineralised. Using SMC could provide plants with S, K, Ca and Mg but there is potential for SO4 2–-S losses via leaching. Received: 7 April 1999  相似文献   

14.
The use of maize (Zea mays L.) genotypes that are able to utilize nutrients efficiently is an important strategy in the management of plant nutritional status; it is of particular importance with regard to potassium (K) and magnesium (Mg), due to their high requirement and influence on plant growth. The influence of K and Mg fertilizers on certain growth parameters of maize genotypes TM.815 and KL.72.AA, including length, seed in ear, seed weight growth, and nutrient concentration, was determined under field conditions over two successive years. The aim of the experiment was to study the effect of different rates of K and Mg fertilizers on maize genotype plant growth parameters, grain yield, and nutrient accumulation under field conditions.

A split plot design with three replicates was used and each block contained three treatments of 0, 100, and 200 kg ha?1 of K2O and 0, 10, and 20 kg ha?1 of Mg; K2SO4 was used to supply K, and MgSO4 was used for Mg.

Plants that responded to the K fertilizer had an increase in height, yield, and the concentration of K in the leaves and seeds. The addition of K fertilizer increased the concentration of nitrogen (N), iron (Fe), zinc (Zn), manganese (Mn), and K in the plant leaves and increased seed K concentration. Mg fertilizer increased the concentration of N, Fe, copper, and Mn in the leaves; however, it exerted no significant influence on K concentration. The KL.72.AA maize genotype had a higher mean plant height, number of seeds in ear, yield, and N, K, Fe, and Zn concentrations compared to the TM.815 maize genotype. In the experiment, the K fertilizer exerted a statistically significant effect on the leaf and seed K concentration; however, on a statistical basis, the Mg fertilizer did not affect the Mg concentration.  相似文献   

15.
Abstract

Most Brazilian soils do not possess sufficient concentrations of available potassium (K) to produce maximum apple yield. Potassium distribution was evaluated with a depth profile of a Humic Xanthic Hapludox receiving K fertilization in an apple orchard, cv. Gala/MM106, at Vacaria, Rio Grande do Sul, Brazil. Treatments consisted of four rates of annual maintenance K fertilization. After 12 years of cultivation, soil was sampled in eight depth increments. Potassium, calcium (Ca), and magnesium (Mg) contents were extracted by Mehlich I, ion‐exchange resin, and ammonium acetate pH 7.0. Long‐term application of K fertilizer resulted in K accumulation mainly in the 0‐ to 30‐cm surface layer, with low K mobilization to deeper layers. Increasing rates of K fertilizer did not affect soil Mg concentration but induced a lower Ca concentration extracted by Mehlich I, especially in the 0‐ to 20‐cm layer. The estimated K2O rate for maximum apple yield was 86.5 kg/ha/year.  相似文献   

16.
二种钾肥对海泡石钝化修复镉污染土壤效应影响的研究   总被引：2，自引：0，他引：2  
为了揭示钾肥对Cd污染土壤钝化修复效果的影响,为土壤钝化修复过程中合理施钾肥提供理论依据。本文选取不同剂量(含量以K2O计算,分别为0.1 g·kg~(-1)、0.2 g·kg~(-1)和0.3 g·kg~(-1))的KCl和K_2SO_4作为典型钾肥,以海泡石(10 g·kg~(-1))作为钝化材料,通过油菜盆栽试验,研究了两种钾肥在海泡石钝化条件下对Cd污染土壤修复效应的影响。结果表明:K_2SO_4显著增加了油菜的生物量,其增幅为6.06%~10.05%。与单施海泡石钝化相比,在海泡石钝化时施用KCl和K_2SO_4两种钾肥,油菜地上部茎叶Cd含量分别增加16.38%~60.73%和15.62%~25.19%;施用KCl和K_2SO_4对土壤p H未产生显著性影响,却显著地增加了土壤有效态Cd含量,其增幅分别为25.51%~34.65%和18.5%~24.96%。添加海泡石可使土壤的Zeta电位向负值方向移动,提高土壤对Cd的负载能力;但添加海泡石下施用KCl和K_2SO_4均能提高土壤的Zeta电位,降低土壤对Cd的负载能力。等温吸附试验同样表明,添加KCl和K_2SO_4均能降低海泡石对Cd的吸附量,在水溶液中海泡石对Cd的最大吸附量为5.30 mg·kg~(-1),添加KCl和K_2SO_4后吸附量分别降低至2.87 mg·g~(-1)和4.92 mg·g~(-1)。KCl和K_2SO_4显著改善了土壤中K、Mn、Cu和Zn等营养元素的有效态含量。从上述结果可以发现,在海泡石钝化修复Cd污染土壤过程中,施K_2SO_4对钝化效果的影响小于施KCl。  相似文献   

17.
Rice straw contains up to 2.3% K in dry matter, including potassium (K) subcompartmented in phytoliths, complex siliceous structures formed in plant tissue via precipitation of Si. Rice straw is usually returned to the soil as a conventional practice to sustain soil nutrients, and therefore, the K pool accompanied with rice straw phytoliths is also cycled. Based on phytoliths obtained by ashing of rice straw at 400 °C and dissolution experiments using batch extraction in combination with physical separation of phytoliths by heavy liquid, this study evaluated the phytolith K(phytK) pool in rice straw and aged phytoliths in paddy soils. Entrapped organic matter containing K within phytolith silica cells was visualized by X-ray tomographic microscopy, and releases of this phytK pool accompanying phytolith dissolution were quantified. A 1% Na2CO3 solution, which has been commonly used to extract amorphous Si and to quantify soil phytoliths, showed obvious responses for K derived from phytolith dissolution, indicating that the Na2CO3 method can be developed for measurement of phytK. In 13 soil samples, Na2CO3-dissolvable K content assignable to phytK was 0.55 ± 0.39 g kg?1 in the puddled horizon, suggesting the phytK pool is of high significance for the management of K in paddy soils.  相似文献   

18.
Abstract

Soil test nutrient concentrations vary with depth, especially in perennial cropping systems where fertilizer is broadcast on the soil surface without incorporation. The objective of this study was to determine the effect of fertilizer rate and sampling depth on soil test phosphorus (P) and potassium (K), and P and K fertilizer recommendations for alfalfa (Medicago sativa L.). Five rates of P and K (0, 56, 112, 224, and 336 kg ha‐1 P2O5 and K2O) were broadcast on established alfalfa stands at three sites with different soil properties and tillage and fertilization histories. In separate plots at one site the same rates of P and K were also incorporated to a depth of 15 cm prior to seeding alfalfa. Soil samples were collected at depths of 0 to 10, 0 to 15, and 0 to 30 cm during the growing season. Fertilizer rates and soil sample depth affected soil test P and K at all sites. Relative to the 30‐cm sample depth, soil test values were higher in fertilized treatments with 10 and 15 cm sample depths due to the concentration of immobile P and K near the soil surface. Sample depths of 10 and 15 cm frequently resulted in lower P and K fertilizer recommendations than those of the 30‐cm depth. Sample depth is an important consideration in routine soil sampling for the purpose of making fertilizer recommendations. If research data used for developing soil test‐based fertilizer recommendation are obtained using a standard sampling depth, routine sampling must also be to the same depth.  相似文献   

19.
Potassium (K) is one of the major mineral elements required for normal growth of cotton. However, understanding the effect of controlled‐release K fertilizer on leaf photosynthesis and K use efficiency (KUE) of cotton is currently limited. A two‐year pot experiment was consecutively conducted in 2014 and 2015 with three kinds of K fertilizer including K2SO4, KCl, and polymer‐coated KCl (CRK), each at four application rates (0.00, 0.86, 1.73, and 2.59 g K plant−1, respectively). For each type of K fertilizer, the yield and K uptake of cotton increased but the KUE decreased with higher K fertilizer application. The release characteristics of K from CRK corresponded well to the K requirements during cotton growth. Plant‐available soil K, as well as leaf SPAD values, net photosynthetic rate (Pn), maximal photochemical efficiency (Fv/Fm), and effective quantum yield of photosystem II (ΦPSII) in CRK treatments were increased after full bloom stage compared to conventional K fertilizers under the same potassium application rate. Consequently, the CRK treatments significantly increased lint cotton yields by 8.1–32.7% and 3.7–20.8%, while the KUE increased by 15.5–54.8% and 14.5–45.4% compared to KCl and K2SO4 treatments, respectively. The results indicate that the application of CRK is intensively recommended to replace conventional potassium fertilizers for gaining greater yields and higher KUE of cotton.  相似文献   

20.
Determining potassium (K) fertilizer requirement using sorption isotherms is considered more accurate than conventional soil K tests. A total of 59 surface soil samples were used to establish K exchange isotherm. To evaluate K requirement sorption test, a glasshouse experiment using perennial ryegrass (Lolium perenne, cv. Roper) was carried out on 10 soil samples. The experiment was laid out as a completely randomized design with four replications and four K levels (K0, K20, K40, K80). Concentrations of K in solution established by adding K in the pots estimated from the sorption curve ranged from 20 to 80 mg K l?1 including check treatment (no K). Dry matter yield of ryegrass in most soils approached maximum as adjusted K levels were increased to 20 mg K l?1. The amounts of K required to bring the soils to 20 mg l?1 in soil solution varied among soils and ranged from 99 to 399 mg kg?1, on average 205 mg kg?1 soil. It was found that a useful regression model for the prediction of standard K requirement (K20) included the combination of plant available K extracted by NH4OAc (Av-K) and clay content: K20 = ?41 ? 0.63 Av-K + 9.0 Clay (R2 = 0.61, p < 0.001, n = 59).  相似文献   

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