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1.
通过室内培养试验,以P/Cd摩尔配比分别为0,2∶3,3∶2,2∶1,4∶1进行了不同磷肥钝化修复Cd污染土壤试验。采用毒性淋溶提取法(TCLP)和形态分析法评价了磷酸氢二铵(DAP)、磷酸二氢钾(MPP)、过磷酸钙(SSP)和磷酸钙(TCP)对污染土壤中Cd的钝化效果。结果表明,4种磷肥的钝化效果依次为:MPPDAPSSPTCP,4种磷肥的钝化处理可显著降低土壤中TCLP提取态Cd含量,在磷肥剂量水平P/Cd为4∶1时对土壤中Cd的钝化效果最佳,最大降低幅度为49%;添加磷肥能够大幅度提高土壤中速效磷的含量,相同磷水平下,土壤中速效磷含量高低次序为:MPPDAPSSPTCP,TCLP提取态Cd含量随土壤速效磷含量升高而显著降低(R=-0.903**);DAP,MPP,SSP和TCP处理后交换态Cd的浓度降幅分别为23.75%,39.06%,16.60%和18.36%,而碳酸盐结合态(WSA)、铁锰氧化物结合态(Fe-Mn-OX)、有机结合态(OM)和残渣态(RES)Cd的含量均有所升高,表明磷素是通过改变Cd的存在形态而降低其有效态含量的。 相似文献
2.
Influence of phosphate on cadmium sorption by calcium carbonate 总被引：1，自引：0，他引：1
Laboratory investigation was conducted to investigate the mechanism of cadmium sorption by pure calcium carbonate and to examine whether, reaction products of phosphate with calcium carbonate serve as a sink for sorption of toxic heavy metal cations like cadmium. The phosphatization of calcium carbonate (G.R) was carried out by treating it with orthophosphoric acid in Ca:P ratio of 5:3, 3:2, 4:3 and 1:1, representing the Ca–P ratios of carbonate apatite, tricalcium phosphate, octacalcium phosphate and dicalcium phosphate and then equilibrated for two months. The X-ray diffraction of the phosphate reaction products revealed that calcite along with monetite, brushite and carbonate apatite were present in each case. The cadmium was effectively retained on CaCO3 by the mechanism of chemisorption at lower Cd2+ concentrations as the pH of the equilibrium system remained constant (8.6) up to initial Cd2+ concentrations of 10−4 mol, coinciding to 100% sorption of Cd2+ from the solution. At higher concentrations, precipitation of CdCO3 on CaCO3 surface or as a separate phase predominated. Enrichment of CaCO3 with P reduced the Cd-sorption. The chemisorption of Cd probably involved the exchange of Ca2+ by Cd2+ from CaCO3 surface. The Cd2+ concentration in equilibrium solution followed the solubility diagram of CdCO3 at pH ≤ 8.6, whereas the concentration of Ca2+ started deviating from the solubility line at pH ≤ 8.2. 相似文献
3.
Radish (Raphanus sativus L.) exhibits a high efficiency in the utilization of sparingly‐soluble phosphates. A greenhouse experiment was designed to investigate the growth response of radish to different phosphorus (P) sources and the nutrient status of the rhizosphere associated with radish growth and nutrient absorption. Radish plants were grown in pots with the roots confined in rhizobags, in such a manner that the concentration of roots was very high within the rhizobag. The rhizosphere soils and non‐rhizosphere soils were analyzed separately for active silicon (Si), aluminum (Al), iron (Fe), and manganese (Mn) using Tamm's solution and for “available”; P using the Bray P1 extraction reagent. The radish growth response was mostly attributable to phosphate amount and availability, and the lime level used in the experiment. Concentrations of active Fe, Si, Al, and Mn were reduced in the rhizosphere, especially when lime and rock phosphate (Ps) were added. Available soil P was accumulated in the rhizosphere under lime and Ps addition, whereas its concentration was reduced with the zero lime treatment. Phosphorus utilization, characterized by P accumulation in shoots, was in accordance with the concentration pattern for “available”; P in the rhizosphere, but not with the growth response of radish itself. The calcium (Ca) concentration of the shoot followed the same trend as the radish growth. There was an antagonism between potassium (K) and Ca absorption as well as between Ca and magnesium (Mg) absorption. With the addition of P, shoot Mn concentration increased, while shoot Fe and Al concentrations increased with no lime addition but decreased with lime addition. The high P efficiency of radish is discussed from the view of rhizosphere chemistry. The high Mn efficiency of radish may be influenced by the same rhizosphere processes that are involved in its high P efficiency. It was concluded that rhizosphere processes and the status of nutrients determined the nutrient efficiency of radish and thus influenced its growth response and nutrient uptake. 相似文献
4.
《Journal of plant nutrition》2013,36(12):2149-2158
Abstract The effects of different commercial phosphate fertilizers [Triple superphosphate (TSP), Tricalcium phosphate (TCP), and ARAD rock phosphate) and soil aluminum (Al) saturation (86, 29, and 0%) on the mineral composition and dry mass production of corn (Zea mays) plants were studied. As soil Al saturation values decreased, pH, calcium (Ca), and magnesium (Mg) levels in the soil increased. High Ca values in the shoot resulted in the reduction in potassium (K) concentrations. The high values of P availability in the soil for the ARAD source of P did not correspond to the high values of dry mass production of corn plants. The high values of corn mass production were noticed for the TSP phosphate source, and the mass productions values were reduced as the soil Al saturation values increased. 相似文献
5.
设施蔬菜大棚土壤氮磷钾养分富积降低土壤钙素的有效性 总被引：5，自引：2，他引：3
6.
The dissolution of a reactive phosphate rock (Gafsa, GPR) was evaluated in a range of UK soils which varied considerably in calcium (Ca) status and in a soil that had been amended with different amounts of a cation exchange resin (CER) to provide a Ca sink of varying size. As expected, but not apparently previously reported, increasing solution Ca concentration caused a decrease in the dissolution of GPR, consistent with the solubility product principle. At 40 d, the extent of GPR dissolution was correlated more closely with soil solution Ca concentration (r=?0.91) than with either the number of unoccupied exchange sites for Ca or the Ca-exchange capacity (CaEC) of the soil (r=0.61 and r=?0.35, respectively). Unoccupied exchange sites for Ca were only effective in influencing GPR dissolution when solution Ca concentration was sufficiently low (< 1 mmol dm?3) for the sites to be operating on the well-buffered portion of the Ca-exchange isotherm. The combined effects of an initial low solution Ca concentration and the presence of unoccupied Ca exchange sites caused the relationship between GPR dissolution and solution Ca concentration to become curvilinear, whereby the proportion of GPR dissolved at 40 d could be related to the initial soil solution Ca concentration by an exponential equation. A similar interaction was obtained for the relationship between GPR dissolution and CaEC (operating at solution Ca concentrations ≥0.6 mmol dm?3) following the addition of CER to the soil. The effectiveness of the additional sites for Ca in maintaining the product of ionic concentrations below the solubility product of GPR was such that the amount of GPR dissolved at 40 d correlated linearly and strongly (r= 1.00) with the CaEC of the soil-CER mixtures. 相似文献
7.
Sutter B Hossner LR Ming DW 《Soil Science Society of America journal. Soil Science Society of America》2005,69(2):362-370
Micronutrient-substituted synthetic hydroxyapatite (SHA) is being evaluated by the National Aeronautics and Space Administration's (NASA) Advanced Life Support (ALS) Program for crop production on long-duration human missions to the International Space Station or for future Lunar or Martian outposts. The stirred-flow technique was utilized to characterize Ca, P, Fe, Mn, and Cu release characteristics from Fe-, Mn-, and Cu-containing SHA in deionized (DI) water, citric acid, and diethylene-triamine-pentaacetic acid (DTPA). Initially, Ca and P release rates decreased rapidly with time and were controlled by a non-SHA calcium phosphate phase(s) with low Ca/P solution molar ratios (0.91-1.51) relative to solid SHA ratios (1.56-1.64). At later times, Ca/P solution molar ratios (1.47-1.79) were near solid SHA ratios and release rates decreased slowly indicating that SHA controlled Ca and P release. Substituted SHA materials had faster dissolution rates relative to unsubstituted SHA. The initial metal release rate order was Mn > Cu > Fe which followed metal-oxide/phosphate solubility suggesting that poorly crystalline metal-oxides/phosphates were dominating metal release. Similar metal release rates for all substituted SHA (approximately 0.01 cmol kg-1 min-1) at the end of the DTPA experiment indicated that SHA dissolution was supplying the metals into solution and that poorly crystalline metal-oxide/phosphates were not controlling metal release. Results indicate that non-SHA Ca-phosphate phases and poorly crystalline metal-oxide/phosphates will contribute Ca, P, and metals. After these phases have dissolved, substituted SHA will be the source of Ca, P, and metals for plants. 相似文献
8.
Antonio Juárez-Maldonado Karim de-Alba-Romenus América Berenice Morales-Díaz 《Journal of plant nutrition》2017,40(13):1908-1919
This study verified the concentration over time of nitrogen, phosphorus, potassium, calcium, magnesium, and sulfur (N, P, K, Ca, Mg, and S) in the leaves, stems, fruits, and roots of tomato plants. An indeterminate growth variety with ball-type fruits suited for greenhouse cultivation was used. The results showed that the distribution of minerals in the different organs of the plant varies over time. The minerals N, P, and K showed a tendency to decrease their concentration, while the concentration of Ca and S increased and that of Mg remained constant over time. The leaves had the highest concentrations of N, P, K, Ca, and Mg. The concentrations of K, for both leaf and stem, ranged between 20 and 30 g kg?1. N and K were the most extracted minerals, while P was the least extracted mineral. The information presented in this paper allows a better fertilization plan for growing tomatoes inside greenhouses. 相似文献
9.
草酸青霉菌HB1溶磷能力及作用机制 总被引：2，自引：0，他引：2
一些功能微生物具有溶磷能力且同一菌株对不同难溶性磷酸盐的溶解能力存在差异。该研究以草酸青霉菌HB1为研究对象,通过固体平板培养试验、摇瓶培养试验和土壤培养试验系统研究了不同磷源(磷酸钙、磷矿粉、磷酸铁、磷酸铝)与氮源(铵态氮、硝态氮)供应下HB1溶磷能力及其作用机制,并验证了其在高、低不同磷水平土壤中的溶磷能力。结果表明,接种HB1的不同磷源培养基上均有溶磷圈出现,根据溶磷圈直径/菌落直径初步确定HB1溶解磷酸钙的能力较强;摇瓶培养试验表明供试磷源为磷酸钙、磷酸铁时HB1发酵液中有效磷含量为884、265 mg/L(铵态氮),或945、206 mg/L(硝态氮),其溶磷能力不受氮源形态影响;磷矿粉为磷源时,HB1发酵液中有效磷含量可达199 mg/L(供应铵态氮),为硝态氮供应的7.14倍;而磷酸铝为磷源时,HB1发酵液中有效磷含量为120 mg/L(供应硝态氮),为铵态氮供应的3.29倍;此外,供应铵态氮条件下,HB1对难溶性磷酸盐的溶解能力与介质中pH值呈显著的负相关关系。HB1接种于不同磷水平的土壤中培养21 d,在低磷和高磷土壤中HB1均能有效定殖且增加了土壤有效磷含量,比不接菌对照分别增加45.00%和14.17%。综上,草酸青霉菌HB1对磷酸钙和磷矿粉的溶磷效果较好,并通过分泌氢质子酸解含磷矿物实现溶磷作用,且HB1在低磷土壤中溶磷能力较强。 相似文献
10.
《Communications in Soil Science and Plant Analysis》2012,43(19-20):2769-2784
Abstract Iron chelates are widely used in fertigation because of their high stability and solubility. However, sudden changes of pH or concentrations of accompanying ions affect chelate stability and make kinetics as relevant as equilibrium data. The kinetics of FeEDDHA and FeEDDHMA reactions at acidic pH values in the presence and absence of calcium (Ca), magnesium (Mg), phosphorus (P), copper (Cu), nickel (Ni), and zinc (Zn) were studied. The FeEDDHA and FeEDDHMA decompound in few seconds at low pH values. The extension of the decomposition reaction is affected by the kind of chelate and concentration. Calcium, Mg, P, Cu, and Zn slightly slow down the reaction. The recovery of both chelates is observed when pH increases. The reaction is quick and practically complete in absence of competing ions, although the percentage of recompound chelate is affected by the chelating agent and pH. FeEDDHMA recompounds in a larger extension than FeEDDHA. The percentage of recompound chelate increases from pH 4 to 7. The rate of reaction and the quantity of recompound chelate are not modified by the presence of Ca or Mg ions. However, phosphate diminishes the percentages of recovery, and its effect is larger as higher is the relationship [P]/[chelate]. The occurrence of Cu, Ni, manganese (Mn), and Zn slows down the reaction at low chelate concentrations. They also decrease the percentage of recompound chelate. The negative effect of the microelements is higher on the recovery of FeEDDHMA than on FeEDDHA, but for both chelates, the influence of the competing ions diminishes as the chelate concentration increases. Copper has the greatest impact on the recomposition of the chelates FeEDDHA and FeEDDHMA, although Ni, a high concentrations, can end up impeding the recovery of FeEDDHMA. 相似文献
11.
Foliar concentrations of starch and major elements, nitrogen (N), phosphorus (P), potassium (K), calcium (Ca), and magnesium (Mg), along with specific leaf weight (SLW) were determined in the potato (Solanum tuberosum L.) cvs 'Denali', 'Norland', and 'Russet Burbank' grown for 35 days under CO2 concentrations of 500, 1,000, 1,500 and 2,000 micromoles mol-1 at both 16 degrees C and 20 degrees C air temperature. The starch concentration, pooled from the three cultivars, increased with increasing CO2 concentration at both 16 degrees C and 20 degrees C and was consistently higher at 16 degrees C than at 20 degrees C. The SLW (g m-2) was positively related to the foliar starch concentration on the basis of leaf area or dry weight. The concentrations of N, P, Ca, and Mg in leaves were negatively related to starch concentration under approximately 14% starch on a dry weight basis. Above 14% starch, there was no significant relationship between element and starch concentrations. Similar patterns were seen when the SLW and element concentrations were expressed on a starch-free basis. In contrast, the leaf concentration of K was not closely related to the starch concentration because the K concentration was similar at varied CO2 levels. The results of this study indicate that the changes in SLW and concentrations of N, P, Ca, and Mg in potato leaves only partially resulted from the changed starch concentration. 相似文献
12.
氮、磷、钾肥与酚对漂洗水稻土硅、铝、铁的活化效应 总被引：1，自引：0，他引：1
本研究以四川盆地西缘茶区漂洗水稻土为供试土壤,采用浸提试验探讨尿素（N）、磷酸二氢钙（P）、硫酸钾（K）和邻苯二酚（Phy）对其硅、铝、铁的活化效应（以浸提液硅、铝、铁的浓度表征）,结果表明: 1）各种处理浸提液均以硅的浓度最大,铝次之,铁最小,即活化效应为硅＞铝＞铁; 2）浸提液硅的浓度为NPK+Phy＞NPK P＞Phy＞K CK N处理,说明磷肥通过磷酸根的配位吸附对其活化产生最重要的影响,同时酚类物质也通过弱酸作用促进其活化; 3）浸提液铝的浓度为NPK+Phy＞Phy＞P NPK K N CK处理,说明酚类物质通过与游离铝形成可溶性络合物而对其活化起突出作用,同时磷肥中的钙离子和钾肥中的钾离子也能将强酸性供试土壤中大量交换性铝离子交换而活化; 4）浸提液铁的浓度为NPK+Phy＞Phy＞K P NPK CK N处理,说明酚类物质通过络合溶铁、还原溶铁等作用对其活化做出重大贡献,同时钾肥中的钾离子和磷肥中的钙离子也将土壤胶体吸附的亚铁离子交换而活化; 5）尿素对漂洗水稻土硅、铝、铁均无显著活化效应。综上所述,磷、钾肥和酚类物质是漂洗水稻土中硅、铝、铁活化的重要影响因素。 相似文献
13.
采用室内模拟施肥、恒温振荡平衡法研究了磷肥种类、磷肥浓度、铅离子浓度、离子强度和酸度影响三峡库区消落带土壤对铅离子的吸附量和解吸量。结果表明：（1）磷肥种类与铅离子的吸附量和解吸量显著相关,施用Ca（H2PO4）2使铅离子的吸附量和解吸量相对较小;（2）土壤铅离子的吸附量和解吸量与施用磷肥浓度呈显著相关,建议选用磷酸二氢钙、磷酸二氢铵、磷酸二氢钾3种磷肥,施用量在3.4066～8.5164kg P2O5·666.6m-2之间较为合适;（3）铅离子浓度极显著地影响土壤吸附和解吸铅离子,随着铅离子浓度的增加,吸附量和解吸量都呈逐渐增加的趋势;（4）离子强度和酸度都极显著地影响土壤吸附和解吸铅离子,建议选用磷酸二氢钙盐、钾盐和铵盐作为磷肥,可以减小土壤铅离子的环境风险。 相似文献
14.
15.
Angel A. Carbonell‐Barrachina Francisco Burló‐Carbonell Jorge Mataix‐Beneyto 《Journal of plant nutrition》2013,36(11):1617-1633
The effects of different levels of arsenic (As) and salinity on bean plant (Phaseolus vulgaris L., cv. Buenos Aires) nutrition were investigated. We studied the processes of absorption and accumulation of macronutrient elements: nitrogen (N), phosphorus (P), potassium (K), calcium (Ca), and magnesium (Mg). The experiment was performed in soilless culture at two levels of As: 2 and 5 mg AsL‐1 (added as sodium arsenite, NaAsO2), and three saline levels [only sodium chloride (NaCl) was added]: 1, 2, and 4 dS‐m‐1. Sodium arsenite and NaCl significantly affected macronutrients allocation within bean plant at concentration levels used in this study. Arsenite depressed K, Na, and Mg concentrations in root, whereas root N, and Ca levels were increased. Nitrogen, P, K, and Na concentrations were significantly higher in As‐stressed plants compared with controls. The addition of NaCl increased Ca concentration in roots and decreased that of K. Salinity tended to increase leaf concentrations of K, Na, Ca, and Mg; whereas leaf N and P levels decreased with increasing salinity. 相似文献
16.
After 100h reaction with Cl-resin and 300h reaction with HCO3-resin (approaching equilibrium), the concentration of anions complementary to phosphate was the critical variable affecting the transfer of P from soil to resin. Solution concentrations of H30+, Ca2+ and phosphate indicated that desorption of P by OH-, and dissolution of Ca phosphates, controlled P release from soils. P extracted by HCO3-resin was much greater than by Cl-resin from an acid soil, due to lower total anion and higher desorbing anion concentrations, but there was little difference between the two resins with a calcareous soil. HCO3-resin extracted a constant proportion of isotopically-exchangeable P from different soils whereas Cl-resin did not. Anion exchange resins provide a convenient means for producing P desorption curves for soils. 相似文献
17.
《Communications in Soil Science and Plant Analysis》2012,43(7-8):573-587
Abstract An agronomic evaluation of phosphate rock and slag on the acid soils of Upata, Bolivar State was conducted to measure their effect on the chemical properties of the soil and growth of Brachiaria decumbens. A field experiment was established using a split plot design with three replications. The treatments were, i) three sources of phosphate rock (Riecito and Lizardo of Falcon State and Monte Fresco of Tachira State) at four rates of P2O5/ha (0, 50, 100, and 200), ii) one source of high‐solubility P [triple superphosphate (TSP) at the same rates], and iii) three levels of calcium applied as basic slag from the Orinoco Steel Company (0, 300, and 600 kg Ca/ha). A basic fertilization was applied to all plots (217 kg/ha Urea, 50 kg/ha KCl, and 78 kg/ha magnesium sulphate). The pasture species used was Brachiaria decumbens. Pasture and soil samples were taken at 2, 3, 5, 7, 12, 14, 16, 17, 24, 27, and 31 months after planting. The pasture samples were analyzed for dry matter production (DM), and percentage content of nitrogen (N), phosphorus (P), potassium (K), calcium (Ca), and magnesium (Mg). Soil samples were analyzed for pH, cation exchange capacity (CEC), and available calcium (Ca) and phosphorus (P). The relative agronomic effectiveness (RAE), calculated using the formula: RAE (%) = DM of the rock ‐ DM of the check plot/DM of TSP ‐ DM of check plot × 100 was applied for each harvest time. The best RAE values at each sampling time were obtained with the Monte Fresco phosphate rock at the rate of 200 kg P2O5/ha and 600 kg Ca/ha as slag. There was a tendency for the RAE value to improve with each sampling apparently due to the slow release of phosphorus from the phosphate rock and its residual effect. There are also values of RAE that show better dry matter production than the high soluble source of TSP. Soil available P and Ca increased with phosphate rock and slag application from 5 and 200 mg/kg to 25 and 400 mg/kg, respectively, after 2.5 years of the experiment. Phosphorus uptake changed from 0.1% in the check plot, which is insufficent to supply the P requirement of grazing cattle in the tropics to a value higher than 0.2%, depending on the sampling time. Soil pH increased slightly from 5.2 to 5.6 with phosphate rock, and to 6.2 when basic slags were applied. 相似文献
18.
施氮水平对富士苹果果实钙形态及品质的影响 总被引：5，自引：2，他引：3
[目的]钙是影响苹果果实品质最重要的元素之一,施氮量影响树体对钙的吸收.探究不同施氮量对果实品质、钙形态以及二者之间的关系的影响,以期为通过科学施肥改善苹果果实品质提供参考.[方法]本研究选择5年生盆栽富士(基砧为组培山定子,中间砧为SH38)为试材,共设6个施氮水平:0(N0)、50(N50)、100(N100)、2... 相似文献
19.
Josefa María Navarro M.Ángeles Botella Antonio Cerdá Vicente Martínez 《Journal of plant nutrition》2013,36(7):991-1006
Melon (Cucumis melo L.) plants were grown hydroponically in a greenhouse to investigate the interaction of phosphorus (P) and calcium (Ca) under saline conditions on vegetative biomass and cation balance. Three levels of Ca (0.4, 2, and 8 mM) were combined factorially with two levels of phosphate (0.1 and 1 mM) under two regimes of NaCl salinity (10 and 80 mM). An increase of phosphate and salinity level decreased shoot and root growth. A strong antagonism between Ca and magnesium (Mg) was observed regardless of the salinity level. Calcium effect on growth depended on the salinity level. At low salinity, an increase of Ca reduced sodium (Na) concentration in all plant fractions. At high salinity, this effect was only significant in young and medium leaves. At low salinity and low Ca the reduction of growth could be due to Na toxicity and an unbalanced Ca/Mg ratio. In addition to that, at high salinity, the restoration of growth by increasing Ca concentration in the root medium could be due to an effect on water relation and by increasing potassium K/Na selectivity. 相似文献
20.
《Communications in Soil Science and Plant Analysis》2012,43(9-10):915-926
Abstract Forage intake with potassium/(calcium + magnesium) [K/(Mg + Ca)] values in excess of 2.2 are associated with grass tetany and Mg deficiencies in ruminants. This study was conducted to determine the degree to which forage K and Mg concentrations and K/(Ca + Mg) ratios could be predicted from soil bicarbonate (HCO3) extractable phosphate‐phosphorus (PO4‐P), and saturation extract Ca, Mg, K, sodium (Na), and nitrate‐nitrogen (NO3‐N) concentrations. Crested wheatgrass (Agropyron spp) strains and cultivars representing four ploidy levels were grown in the greenhouse on eight calcareous soils with different saturation extract Ca, Mg, K and K/Mg ratios. The plants were harvested three times. Soil solution K/(Ca + Mg) and K/Mg ratios were the only measured soil parameters that showed a consistent correlation with plant K/(Ca + Mg) ratios. Bicarbonate extractable soil P was positively related to plant P and K uptake in the first harvest, but was not related in the second and third harvests nor was soil P related to plant Ca or Mg content. There was a tendency for the higher ploidy level entries to have higher plant K/(Ca + Mg) ratios. It was concluded that soil K/(Ca + Mg) ratios can be used to predict relative forage K/(Ca + Mg) ratios for grasses grown under similar conditions. 相似文献