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991.
采用水扬酸 -硫酸 -锌粉还原 ,双氧水作消化加速剂处理复合肥有机肥样品 ,测定N、P、K含量 ,结果与其它分析方法差异很小 ,回收率较高 ,是一种方便、快速测定复合肥、有机肥和其它肥料全量N、P、K的测试方法 相似文献
992.
石灰性土壤施用不同磷肥对玉米苗期生长和土壤无机磷组分的影响 总被引:2,自引:0,他引:2
研究旨在探讨不同磷肥品种对玉米生长发育和土壤无机磷组分的影响,以期为磷肥高效利用提供参考。采用盆栽试验,设置6个处理:磷酸一铵(MAP)、过磷酸钙(SSP)、聚磷酸铵(APP)、氮磷复合肥硝酸磷肥(NiP)、硫酸铵+过磷酸钙混施(SA+P),试验60天后测定了玉米的生物学指标和玉米植株磷素含量,同时测定了土壤有效磷与土壤无机磷组分含量状况。结果表明:玉米生物学性状、磷素累积量和磷肥利用效率均表现出APPMAP、NiPSSP、SA+PCK的趋势。相较于对照,APP、MAP、NiP处理显著提高玉米植株的株高、叶面积、地上部和根系干重,株高增幅在23.3~35.1 cm,叶面积增加57.1~89.0 cm~2,地上部和根系干重分别增加265%~420%和171%~218%。APP处理植株磷素累积量达到49.02 mg/盆,磷肥利用效率达到36.75%,显著高于NiP和MAP的21.43%和19.42%。相较于对照,APP和MAP处理的Ca_2—P、Ca_8—P和Fe—P呈显著性增加,上述3种无机磷组分含量与玉米植株磷累积量呈极显著正相关关系(p0.001)。北方石灰性土壤聚磷酸铵(APP)是一种表现良好的磷肥类型,这对减磷增效背景下的粮食安全和磷肥高效利用有重要应用价值。 相似文献
993.
994.
995.
不同类型有机物料的有机磷组成及生物有效性 总被引:2,自引:1,他引:1
996.
Phosphorus accumulation and leaching risk of greenhouse vegetable soils in Southeast China 总被引:4,自引:0,他引:4
Yusef KIANPOOR KALKHAJEH Biao HUANG Helle S?RENSEN Peter E. HOLM Hans Christian B. HANSEN 《土壤圈》2021,31(5):683-693
Over-fertilization has caused significant phosphorus(P) accumulation in Chinese greenhouse vegetable production(GVP) soils. This study, for the first time, quantified profile P accumulation directly from soil P measurements, as well as subsoil P immobilization, in three alkaline coarse-textured GVP soil profiles with 5(S5), 15(S15), and 30(S30) years of cultivation in Tongshan, Southeast China. For each profile, soil samples were collected at depths of 0–10(topsoil), 10–20, 20–40, 40–60, 60–80, and 80–100 cm. Phosphorus accumulation was estimated from the difference in P contents between topsoil and parent material(60–100 cm subsoil). Phosphorus mobility was assessed from measurements of water-soluble P concentration(PSol). Finally, P sorption isotherms were produced using a batch sorption experiment and fitted using a modified Langmuir model. High total P contents of 1 980(S5), 3 190(S15), and 2 330(S30) mg kg~(-1) were measured in the topsoils versus lower total P content of approximately 600 mg kg~(-1) in the 80–100 cm subsoils. Likewise, topsoil PSol values were very high, varying from 6.4 to 17.0 mg L~(-1). The estimated annual P accumulations in the topsoils were 397(S5), 212(S15), and 78(S30) kg ha~(-1) year~(-1). Sorption isotherms demonstrated the dominance of P desorption in highly P-saturated topsoils, whereas the amount of adsorbed P increased in the 80–100 cm subsoils with slightly larger P adsorption capacity. The total P adsorption capacity of the 80–100 cm subsoils at a solution P concentration of0.5 mg L~(-1) was 15.7(S5), 8.7(S15), and 6.5(S30) kg ha~(-1), demonstrating that subsoils were unable to secure P concentrations in leaching water below 0.5 mg L~(-1) because of their insufficient P-binding capacity. 相似文献
997.
Biodiversity, current developments and potential biotechnological applications of phosphorus-solubilizing and -mobilizing microbes: A review 总被引:3,自引:0,他引:3
Divjot KOUR Kusam Lata RANA Tanvir KAUR Neelam YADAV Ajar Nath YADAV Manish KUMAR Vinod KUMAR Harcharan Singh DHALIWAL Anil Kumar SAXENA 《土壤圈》2021,31(1):43-75
As one of the most important and essential macronutrients next to nitrogen,phosphorus(P)is important for plant development,but it is the least mobile nutrient element in plant and soil.Globally,P is mined from geological sediments and added to agricultural soils so as to meet the critical requirements of crop plants for agronomic productivity.Phosphorus exists in soil in both organic and inorganic forms.The various inorganic forms of the element in soil are salts with calcium,iron,and aluminum,whereas the organic forms come from decaying vegetation and microbial residue.There is a huge diversity of plant microbiomes(epiphytic,endophytic,and rhizospheric)and soil microbiomes that have the capability to solubilize the insoluble P and make it available to plant.The main mechanism for the solubilization of inorganic P is by the production of organic acids,which lowers soil pH,or by the production of acid and alkaline phosphatases,which causes the mineralization of organic P.The P-solubilizing and-mobilizing microorganisms belong to all three domains,comprising archaea,bacteria,and eukarya.The strains belonging to the genera Arthrobacter,Bacillus,Burkholderia,Natrinema,Pseudomonas,Rhizobium,and Serratia have been reported as efficient and potential P solubilizers.The use of P solubilizers,alone or in combination with other plant growth-promoting microbes as an eco-friendly microbial consortium,could increase the P uptake of crops,increasing their yields for agricultural and environmental sustainability. 相似文献
998.
In agricultural systems, it is vital to use limited yet optimal phosphorus(P) resources, because excessive P fertilizer application leads to the accumulation of P in soil, increasing the risk of environmental pollution and causing the waste and exhaustion of P resources. In a rice-wheat rotation system, omitting P fertilizer application in the rice-growing season is a good alternative;however, how this P fertilization reduction influences changes in P in the soil-root-aboveground system is unclear. In this study, after a seven-year rice-wheat rotation at the Yixing(YX) and Changshu(CS) sampling sites, China, compared with P fertilization in rice-and wheat-growing seasons(PR+W), reduced P fertilization(no P fertilizer application in either season, P0;P fertilization only in wheat-growing seasons, PW;and P fertilization only in rice-growing seasons, PR) did not result in substantial variation in crop biomass. The PW treatment did not reduce crop total P, root iron(Fe)-plaque P, and soil Olsen-P at three stages of rice growth(seedling, booting, and harvesting stages) at the YX and CS sites. In contrast, concentrations of soil Olsen-P, aboveground crop total P, and root Fe-plaque P decreased in the P0 treatment by 45.8%–81.0%,24.6%–30.9%, and 45.6%–73.4%, respectively. In addition, a significant negative correlation was observed between the root Fe-plaque P and crop biomass at the two sites. Significant positive correlations were also observed between root Fe-plaque P and root total P, crop total P, and soil Olsen-P. In addition, the results of a redundancy analysis revealed that soil alkaline phosphatase(ALP) played a major role in the supply of P in soil, and was closely associated with root Fe-plaque P. The results of this study will enhance the understanding of the changes in P in the soil-root-aboveground system, particularly under P fertilizer reduction regimes. 相似文献
999.
应用高效液相色谱,对华北地区某水库5个采样点水体中微囊藻毒素(MC-LR、RR和YR)3种异构体进行了为期1a的监测,研究3种异构体随时间的变化规律及相互关系。结果表明,水体中3种异构体(-LR、YR和RR)含量分别为0.941±1.338、0.365±0.647和(2.893±5.387)μg·L-1;3种异构体出现时间不一样,LR异构体出现时间最早,在4月下旬即可检测到,而RR和YR异构体则需到5月中旬才能检测到;3种异构体峰值出现时间也不一致,LR和YR异构体峰值出现在8—9月,而RR异构体出现时间较晚,到10—11月才达到全年最高值;LR和RR异构体的含量比较高,是主要毒素,5—11月,其比值由2.20降到0.04,这与水体中的N/P比值有关,它随N/P比值的减少而减少。 相似文献
1000.
浙北平原不同种植年限蔬菜地土壤氮磷的积累及环境风险评价 总被引:1,自引:0,他引:1
长期过量施肥可导致蔬菜地土壤养分大量累积、养分利用效率下降和环境污染风险增加。以浙北平原不同种植年限蔬菜地土壤为研究对象,采用化学测试方法研究了菜地土壤氮和磷的积累及其淋失潜力的变化。结果表明,随着种植年限的增加,蔬菜地土壤全磷、有效磷(Olsen P)和NO3-N呈明显的积累;蔬菜种植年限为〈2、2~5、6~10、11~20、20~30和>30a的表土全P平均分别为0.66、0.75、1.07、1.49、2.40和2.12g·kg-1,有效P平均分别为13.2、37.8、42.2、70.2、137.9和101.7mg·kg-1,NO3-N平均分别为9.15、13.58、50.18、46.48、73.28和74.20mg·kg-1,同时土壤N和P垂直下移渐趋明显。土壤水溶性磷含量随土壤有效磷(OlsenP)积累的变化存在一个明显的突变点,相对应的土壤OlsenP临界值约为60mg·kg-1。随着种植年限增长,蔬菜地地表径流中氮和磷浓度呈明显增加,利用年限为20~30a的蔬菜地径流中可溶性P和NO3-N浓度分别约为利用年限〈2a蔬菜地的13.12和9.48倍。研究认为,长期超量施肥已导致这一地区蔬菜地土壤养分的过度积累,在蔬菜生产中应重视和提倡平衡施肥,控制土壤氮磷的积累。 相似文献