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991.
992.
本文研究了磷灰石的结晶性质,包括CO32-与PO43-的置换量、a0、c0、Da0、Dc0和CO2指数,和磷矿粉直接施用肥效的相关性。结果表明,101个磷灰石的晶格中,CO2%的变幅为3.62-0.04%;a0为9.331-9.380A;c0的变幅比较小;Da0为391-2242A;Dc0为424-2000A;CO2指数为0.000-0.493。磷矿粉肥效与磷灰石结晶参数的相关阵表明,CO2置换量的多少与磷灰石的组成最为相关(r=0.999)。这是氟磷灰石被碳酸根置换后形成碳氟磷灰石的理论依据。同时,CO2与a0、Da0和Dc0均呈极显著的负相关。逐步回归分析表明,上述各个参数中,对磷矿粉增产起主导作用的是Da0和Dc0,即最能评价磷矿粉肥效高低的是磷灰石晶粒的比表面大小。2%柠檬酸直接浸提原磷矿时,受到磷矿中伴生的碳酸盐矿物的干扰,其中方解石的干扰显著大于白云石。对于提纯的磷矿,由于碳酸盐的干扰已经消除,因而其与磷矿粉肥效的相关系数的可靠性可以提高到2倍左右。 相似文献
993.
石灰性土壤无机磷的形态分布及其有效性 总被引:66,自引:1,他引:66
本文应用蒋柏藩和顾益初(1989)提出的石灰性土壤无机磷的分级方法,对我国北方主要的石灰性土类进行了无机磷形态分级的研究,并对其有效性作出了初步评价。供试的甘肃、陕西和河南的16种土壤的无机磷形态的分布情况为:Ca2-P平均占无机磷总量的1.34%,Ca-P占9.91%,Al-P占4.27%,Fe-P占4.40%,O-P占10.9%,Ca10-P占69.1%。生物试验的结果表明:Ca2-P型的磷酸盐是最有效的,也是作物磷素营养的主要来源;Ca8-P、Al-P和Fe-P可以作为缓效磷源;Ca10-P和O-P只是一种潜在磷源。本研究为石灰性土壤无机磷的研究和磷肥的合理施用提供了理论依据。 相似文献
994.
一种基于NIR-RED光谱特征空间的干旱监测新方法 总被引:1,自引:0,他引:1
土壤水分作为干旱监测的重要指标,一直是干旱遥感监测研究的重要内容。本研究利用MODIS数据的EVI、红波段反射率、近红外波段反射率数据构建了基于Nir-Red反特率光谱特征空间的EPDI模型进行土壤水分的反演。利用野外同步测量数据对PDI、MPDI、EPDI三种干旱指数模型获取的拉萨河流域土壤水分进行了验证和对比分析,研究结果表明EPDI能够更准确地反演土壤水分,其样本点的相对误差仅为0.1040,线性相关系数为0.9181,反演精度相比PDI、MPDI(0.1646、0.1472)分别提高了36.83%和29.35%,为利用遥感影像数据进行大尺度的干旱动态监测提供了新途径。并且相比MPDI,EPDI模型参数更容易获取,模型构建受人为因素影响小,从而为模型的大范围推广提供了可能,具有很好的应用意义。 相似文献
995.
Jia X. Xiao Cheng Y. Hu Ying Y. Chen Jun Hua Bo Yang 《Journal of plant nutrition》2015,38(10):1516-1529
A pot experiment was conducted to examine the effects of arbuscular mycorrhizal fungi, Glomus versiforme, G. mosseae, and G. intraradices on growth and nutrition of trifoliate orange (Poncirus trifoliata) seedlings under magnesium (Mg)-nontreated and Mg-treated conditions. Whether treated with Mg or not, G. versiforme inoculation significantly enhanced the growth and concentrations of Mg, phosphorus, calcium, potassium, zinc, and copper in shoots or roots, and activities of acid phosphatase, catalase, invertase, and urease in rhizosphere soils. Additionally, there were higher levels of chlorophyll, proline, soluble sugar and protein in leaves, root viability, superoxide dismutase, peroxidase and catalase in leaves and roots, but lower malondialdehyde content in leaves and roots of mycorrhizal seedlings than non-mycorrhizal ones. Data demonstrated that G. versiforme-inoculated citrus seedlings exhibited higher levels of soil enzymes, osmoregulation, and antioxidant matters, leading to improvement of growth and nutrition of seedlings in low Mg soil. 相似文献
996.
997.
Increased degradation of phenanthrene in soil by Pseudomonas sp. GF3 in the presence of wheat 总被引:1,自引:0,他引:1
A phenanthrene-degrading bacterial strain Pseudomonas sp. GF3 was examined for plant-growth promoting effects and phenanthrene removal in soil artificially contaminated with low and high levels of phenanthrene (0, 100 and 200 mg kg−1) in pot experiments. Low and high phenanthrene treatments significantly decreased the growth of wheat. Inoculation with bacterial strain Pseudomonas sp. GF3 was found to increase root and shoot growth of wheat. Strain GF3 was able to degrade phenanthrene effectively in the unplanted and planted soils. Over a period of 80 days the concentration of phenanthrene in soil in which wheat was grown was significantly lower than in unplanted soil (p<0.05). At the end of the 80-d experiments, 62.2% and 42.3% of phenanthrene had disappeared from planted soils without Pseudomonas sp. GF3 when the phenanthrene was added at 100 and 200 mg kg−1 soil, respectively, but 84.8% and 70.2% of phenanthrene had disappeared from planted soils with the bacterial inoculation. The presence of vegetation significantly enhances the dissipation of phenanthrene in the soil. There was no significant difference in soil polyphenol oxidase activities among the applications of 0, 100 and 200 mg kg−1 of phenanthrene. However, the enzyme activities in planted and unplanted soils inoculated with the strain Pseudomonas sp. GF3 were significantly higher than those of non-inoculation controls. The bacterial isolate was also able to colonize and develop in the rhizosphere soil of wheat after inoculation. 相似文献
998.
G. Zhang G. M. Zeng Y. M. Jiang J. M. Yao G. H. Huang X. Y. Jiang W. Tan X. L. Zhang M. Zeng 《Water, air, and soil pollution》2006,172(1-4):39-55
The effects of Weak acids (WA) on the canopy leaching and uptake processes are evaluated by comparing the leached base cations or the absorbed protons while including and excluding WA, e.g. the WA-included method and the WA-excluded method. The seasonal WA throughfall flux is even larger than twice the bulk precipitation flux except summer, which not only partly agrees with the conclusion that the total deposition of WA equals twice the bulk or dry deposition flux in European Intensive Monitoring plots (level II), but also indicates the significant canopy leaching of WA in Shaoshan forest. The seasonal canopy leaching of base cations in association with WA accounts for 6–30% of the total base cations in throughfall, with an annual mean of 23%, which is slightly higher than the 15% at the Speulder forest in The Netherlands. The canopy exchange capacity of H+ to NH4 + is closed to 6.0 while neglecting the WA exchange, which probably supports the assumption that the exchange capacity of H+ is six times that of NH4 +. Simultaneously, we suggest that the WA is competitive to a certain extent with protons to leach base cations of plant tissues during the canopy exchange processes. 相似文献
999.
[目的] 研究辽西北沙地农林复合系统土壤养分的空间分布及其效应,从土壤养分角度探讨果农间作系统中果树和农作物对土壤养分的相互作用关系,为该区农林复合系统的可持续经营提供科学合理的依据。[方法] 以苹果与花生间作、花生单作、苹果单作为研究对象,对0-60 cm土层深度,0-300 cm水平距离范围内土壤养分含量进行测定和分析。[结果] 沙地间作系统中土壤有机质、速效钾极缺乏,全氮、碱解氮很缺乏,全磷缺乏,有效磷含量中等;间作系统在水平方向上,苹果树和花生植株对总养分有机质、氮、磷的竞争激烈位点位于果树带区,对有效养分氮、磷、钾的竞争激烈位点位于近果树作物区;在垂直方向上,各养分总体表现出了表聚性,间作系统对有机质、有效磷的竞争主要位于深土层,对全磷、速效钾的竞争主要位于表土层,对全氮、碱解氮表现为合作效应,表土层效应更高;与苹果单作、花生单作相比较,间作系统速效钾和有效磷含量呈现负效应。[结论] 沙地苹果-花生间作系统土壤养分贫瘠,应在果树带区施用有机肥、磷肥,作物区施入钾肥,以减轻养分竞争,提高养分效应。 相似文献
1000.
X. Z. Xu H.‐W. Zhang G.‐Q. Wang Y. Peng O. Y. Zhang 《Land Degradation \u0026amp; Development》2006,17(6):629-644
The building of check‐dams is one of the most effective measures for the conservation of soil and water in the Loess Plateau of China, and the hydro‐sedimentologic balance is the most important factor influencing the relative stability of the check‐dam systems. This means that the soil and water in small watersheds controlled by the check‐dams will be absorbed internally, without the need for raising the height of the dams, if some given parameters have reached certain values. A runoff simulation experiment for a single check‐dam and a rainfall simulation experiment for the whole check‐dam system has been conducted, and the runoff/rainfall intensity and the parameter RV were determined through the annual erosion rate of the prototype watershed. The results indicated that the raising of the dam‐land altitude became slower, and the mean gradient of the gully was kept at a constant. The main reasons causing the check‐dam to show a good relative stability are the enlarging of the dam‐land area, the alleviating of erosion by the check‐dam, and the auto‐stabilizing mechanism of the gullies. This study presents a kind of scale‐down model experiment in which the ratio of the model geomorphological variable to the corresponding prototype variable keeps constant after the determinate runs of rainfalls, so that the soil and water erosion processes of the prototype could be monitored from the results of the model experiment. Four measures have been suggested for ensuring this ratio is a constant: (1) A bare‐land model with an appropriate erosion rate should be used in the experiment. (2) Dimensions of the landform, including the check‐dam, should normally be scaled down according to the prototype watershed. (3) Soil similar to those of the prototype should be used. (4) The antecedent water content before each rainfall simulation should be kept constant. Copyright © 2006 John Wiley & Sons, Ltd. 相似文献