酸性低钾土硫酸钾镁肥对花生生长及养分吸收的影响

在供钾水平较低的酸性赤砂土上,采用盆栽试验方法研究硫酸钾镁对花生生长发育及养分吸收的影响,结果表明:随硫酸钾镁用量的增加,花生经济产量与生物总量呈先增加后降低的趋势.施硫酸钾镁513mg·kg-1(土)处理(相当于每千克土施K2O 0.12 g、Mg 0.028 g、S 0.09 g),花生产量最高,经济产量与生物总量分别较对照增加20.2%和32.2%.随硫酸钾镁用量的增加,植株对钾、镁、硫各吸收量均有不同程度增加,其中对钾、硫吸收量呈逐渐升高的趋势,而对镁吸收量呈先升高后降低的趋势,植株对钾、镁吸收表现正相关.随硫酸钾镁用量的增加,花生果仁粗蛋白与粗脂肪均较对照有所提高,粗蛋白含量呈逐渐增加,而粗脂肪含量却呈逐渐下降趋势.在酸性低钾、中镁、潜在性缺硫的赤砂土上,花生施用硫酸钾镁肥,钾镁养分吸收里显著正相关,但钾硫相关性不明显.     

硫酸钾镁肥在马铃薯上的肥效试验研究

进行硫酸钾镁肥在马铃薯上的肥效试验研究,结果表明:磷酸二铵450 kg/hm2+尿素75 kg/hm2+硫酸钾镁肥300 kg/hm2的处理马铃薯产量最高,磷酸二铵450 kg/hm2+尿素75 kg/hm2+硫酸钾镁肥225 kg/hm2的处理施肥投入成本较低,经济效益最佳。     

硫酸改性沸石中主要交换性阳离子动态变化研究

近年来天然沸石在农业中得到了广泛的应用.利用硫酸对天然沸石进行活化试验,通过对其1年的动态监测,分析沸石中对植物生长有重要影响的交换性K+、Ca2+、Mg2+、Na+以及阳离子交换量动态变化,以得到硫酸和沸石反应后各养分的动态变化,为改性后沸石生产农作物矿物肥提供理论依据.     

镁、锰、活性炭和石灰及其交互作用对小麦镉吸收的影响

采用盆栽试验,研究了在镉污染土壤上施用石灰、硫酸镁、硫酸锰和活性炭不同用量以及交互作用对小麦生长和吸收重金属镉的影响。研究结果表明,在试验条件下施用适量的硫酸镁、硫酸锰或与石灰配合能明显提高小麦籽粒产量,单施石灰或与活性炭配合施用降低了小麦籽粒产量;与对照(CK)相比, 所有处理秸秆产量均下降。施用硫酸镁能显著降低小麦籽粒和秸秆中Cd浓度,且随用量的增加而增大。低量硫酸锰能有效降低小麦籽粒和秸秆中Cd浓度,高量反而增加小麦对Cd的吸收。石灰、活性炭单独施用或配合施用都能明显减少小麦对Cd的吸收,但籽/杆中Cd比却随石灰用量的增加呈明显的上升趋势。叶面喷施硫酸镁对降低小麦吸收镉的效果与土施相当,但叶面喷施硫酸锰却比土施硫酸锰显著降低了小麦籽粒中的镉浓度与吸收量。硫酸镁与硫酸锰,或石灰、硫酸镁和硫酸锰3种物质配合施用,对小麦籽粒镉浓度和吸收量的降低表现出明显的正交互作用,对抑制小麦体内镉从秸秆向籽粒的转移具有显著效果。     

钾镁水平对番茄苗期生长、根系形态及钾素吸收和生理利用效率的影响

采用水培方法,研究不同钾、镁水平对"天福冠露"和"毛粉802"两种番茄幼苗生长、根系特征及钾素吸收、利用效率的影响。结果表明,钾、镁水平(8 mmol/L、1 mmol/L)处理的植株鲜重、干重及钾、镁水平(4 mmol/L、4 mmol/L)处理的株高显著高于其他处理。随钾、镁水平升高,两种番茄植株的根长、"天福冠露"植株的根直径、根体积和分根数先减少后增加;番茄植株钾素吸收率显著提高,生理利用效率显著降低。钾、镁水平(8 mmol/L、1 mmol/L)处理的植株根长、根表面积、根直径及根体积显著高于缺钾处理。钾、镁水平(4 mmol/L、4 mmol/L)处理,两种番茄植株根长、根表面积、根体积和分根数均显著高于缺镁处理,"天福冠露"植株钾含量显著高于"毛粉802",而钾素生理利用效率显著低于"毛粉802"。与其它等钾处理相比,缺镁植株钾素积累量最低、生理利用效率最高,镁过量处理的植株钾素生理利用效率显著降低。     

Increase in the Capacity of Interlayer Sites in a Paddy Soil as a Possible Factor Affecting the Dynamics of Fixed Ammonium at the Initial Stage of Anaerobic Incubation

To evaluate whether the capacity of interlayer sites affects the dynamics of fixed ammonium (NH₄⁺) in a paddy soil, a combination of potassium (K)–saturation treatment and stepwise extraction of nonexchangeable K with 0.01 mol L^?1 hydrochloric acid was applied to a soil incubated anaerobically up to 70 days. The capacity of interlayer sites increased with an increase of weakly fixed NH₄⁺ during the initial 28 days (r = 0.78, P < 0.01), and remained stable thereafter. On the other hand, the concentration of exchangeable NH₄⁺ increased curvilinearly during the whole incubation period, which was correlated with an increase of weakly fixed NH₄⁺ (r = 0.85, P < 0.01). These results suggested that the dynamics of weakly fixed NH₄⁺ in a paddy soil is regulated not only by the chemical equilibrium between exchangeable and weakly fixed NH₄⁺ but also by the capacity of interlayer sites within a few weeks after flooding.     

Improving Soil Fertility to Support Grass–Legume Revegetation on Lignite Mine Spoils

The short-term sequential effects of different treatments on soil fertility and revegetation of mine spoils were examined in a lignite mine in northwestern Spain. Experimental plots were established both on old and recent spoils after tillage and treated with compost or nitrogen (N), phosphorus (P), potassium (K), + magnesium limestone before seeding with a grass–legume species mixture. Compost improved plant production and, contrary to NPK, maintained soil N levels and supplied enough P for the establishment and early growth of the vegetation. Severe magnesium (Mg), calcium (Ca), and K limitations in recent spoils were only alleviated by compost + magnesium limestone, allowing the rapid growth and coating of the soil surface. The amendment based on NPK + magnesium limestone improved plant production in the short term but caused proliferation of weeds. Results suggest that revegetation in combination with the appropriate amendments is a key issue for the reclamation of lignite mine spoils.     

Interrelationships between soil magnesium forms

Abstract

A second order equation best described the relationship between exchangeable Mg and both total and acid‐soluble Mg in select temperate and tropical soils. The relationship between acid‐soluble and total Mg was linear. Soil types differ in their Mg contents. On a per unit weight of material bases the finer soil particles contained more than 95 percent of the total soil inorganic magnesium. In tropical soils, as in temperate soils, the total Mg content of surface horizons tends to decrease with severe weathering, soil erosion and movement of soil colloidal particles down the profile.     

Principles underlying the practice of determining lime requirements of acid soils by use of buffer methods

Abstract

A buffer is generally a mixture of a weak acid and a salt of the same weak acid. Hence it can neutralize both acids and bases, and thus resists marked changes in pH of a system. Yet systematic change in pH of a buffer caused by addition of an acidic substance can be used to indicate the total acidity represented by the change in buffer pH. Since acid soil is itself a buffer, when it is added to a buffer mixture for the purpose of measuring its acidity or lime requirement (LR), the resulting double‐buffer suspension (soil‐buffer) is a relatively complex system. Much of the complication in interpreting the changes in buffer pH brought about by mixing soil and buffer stems from the facts: i) that much of the acidity is pH‐dependent, and ii) that quick‐test methodology involves reaction of only a fraction of the total soil acidity with the buffer. Marked change in relative amounts of H ions dissociating from the soil‐SMP‐buffer system at soil‐buffer pH 6.9 and above accounts for relatively wide variations between buffer‐indicated and CaCO₃ incubation‐measured LR of low LR soils. Similarly, decreased reactivity of H⁺ in high organic matter soils and increased reactivity of H in acid‐leached soils cause errors in buffer‐indicated LR. Awareness of these principles helps avoid pitfalls of existing buffer methods, and has led to incorporation of the double‐buffer feature for improving the SMP method.     

Doybean growth and composition as affected by K,Ca, and Mg rates and corn rotation

Abstract

Different rates of K, Ca, and Mg were applied to bulklots of Decatur clay loam (pH 5.8) which had been collected from an area under natural vegetation. Nitrogen and P were each applied at the rate of 100 ppm. Soybean (Glycine max L.) and corn (Zea mays L.) were planted to pots in four replications of each treatment. Plants were grown for 6 weeks and subsequently all the pots were re‐planted to soybeans. This crop rotation was repeated until six crops had been harvested from each pot.

Potassium fertilization did not affect soybean growth but increased the dry matter of corn plants. Calcium application affected the growth of neither crop, but Mg addition to the soil reduced the growth of both crops. The composition of the plants generally reflected the available amounts of each nutrient. Additionally, Mg consistently decreased K in soybeans but increased Mn in the two crops. The inclusion of corn in rotation with soybeans resulted in the following effects on the succeeding soybean harvests: more tolerance to high Mg, greater reduction of plant Ca and Mg caused by K application, and lower levels of available K and Ma in soils and soybeans. However, the greater rate of depletion of soil K and Mn under corn rotation did not appear Co affect the dry matter yields of the following soybean plants relative to the plants under the continuous soybean cropping system.