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Impact of flue gas desulfurization-calcium sulfite and gypsum on soil microbial activity and wheat growth

机译:烟气脱硫-亚硫酸钙和石膏对土壤微生物活性和小麦生长的影响

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Calcium sulfite (CaSO3 center dot 0.5H(2)0), a common by-product of coal combustion and flue gas desulfurization (FGD), spontaneously converts to gypsum (CaSO4 center dot 2H(2)0) with exposure to air and water. Although gypsum is a well-known soil amendment, the oxidation of SO32- to SO42- consumes oxygen and may have detrimental effects on plant root growth and soil microbial activity if FGD-CaSO3 is land applied. Because the oxidation rate is pH dependent, we conducted greenhouse tests to evaluate the effects of FGD-CaSO3 applied at rates of 0, 2.2, 4.4, and 8.8 Mg ha(-1) on wheat growth, soil enzyme activities, and the chemical properties of two soils with differing pH (4.0 vs. 6.2). A gypsum treatment applied at the rate of 2.2 Mg ha(-1) was used as a positive control. Exchangeable Ca2+ and water-extractable Ca2+ and 2 increased significantly with increasing FGD-CaSO3 application SO42- increased in both soils, indicating rapid oxidation Of SO32- to SO42- when neither water nor oxygen was limiting. No changes in I soil pH were measured. Applications of 2.2, 4.4, or 8.8 Mg CaSO3 ha to the pH 6.2 soil produced no effect on wheat growth or the uptake of N, P, Ca2+, and Mg2+. The uptake Of SO42- -S increased, whereas K uptake decreased. No significant differences in the activities of urease, beta-glucosidase, alkaline phosphatase, or arylsulfitase were observed relative to a control. In the acid soil, an application of 2.2 Mg ha(-1) FGD-CaSO3 increased wheat root growth and dry matter yield compared with an untreated control. The uptake of N, P, Ca2+, and K+ also increased presumably because of enhanced root development resulting from decreases in exchangeable Al3+ and increases in soluble Ca2+. Wheat growth and alkaline phosphatase and arylsulfatase activities were significantly inhibited by addition of 8.8 Mg ha(-1) of FGD-CaSO3 compared with the untreated control or the same soil receiving 2.2 Mg ha(-1) gypsum. We conclude that surface applications of FGD-CaSO3 may be as effective as gypsum for inhibiting soil crusting, improving water infiltration, and promoting the movement of Ca2+ into acid subsoils. Moreover, application rates of equal to or less than 4.4 Mg ha-1 should have no negative impact on soil microbial activities or plant growth.
机译:亚硫酸钙(CaSO3中心点0.5H(2)0)是煤燃烧和烟气脱硫(FGD)的常见副产品,在暴露于空气和水后会自发转化为石膏(CaSO4中心点2H(2)0) 。尽管石膏是一种众所周知的土壤改良剂,但是如果在土地上施用FGD-CaSO3,则SO32-氧化为SO42-会消耗氧气,并且可能对植物根系生长和土壤微生物活性产生不利影响。由于氧化速率取决于pH值,我们进行了温室测试,以评估以0、2.2、4.4和8.8 Mg ha(-1)施用FGD-CaSO3对小麦生长,土壤酶活性和化学性质的影响。 pH值不同的两种土壤(4.0和6.2)。以2.2 Mg ha(-1)的速率施用的石膏处理用作阳性对照。随着FGD-CaSO3施用量的增加,可交换Ca2 +和可水提取的Ca2 +和2均显着增加,两种土壤中SO42-均增加,表明当水和氧气均不受限制时,SO32-迅速氧化为SO42-。没有测量土壤pH值的变化。在pH值为6.2的土壤上施用2.2、4.4或8.8 Mg CaSO3 ha对小麦的生长或N,P,Ca2 +和Mg2 +的吸收均无影响。 SO42- -S的吸收增加,而K的吸收减少。相对于对照,未观察到脲酶,β-葡萄糖苷酶,碱性磷酸酶或芳基亚硫酸酯酶的活性的显着差异。在酸性土壤中,与未经处理的对照相比,施用2.2 Mg ha(-1)FGD-CaSO3可增加小麦根的生长和干物质产量。推测N,P,Ca2 +和K +的吸收也增加了,这是由于可交换Al3 +的减少和可溶性Ca2 +的增加导致了根的发育增强。与未处理的对照或接受2.2 Mg ha(-1)石膏的相同土壤相比,添加8.8 Mg ha(-1)的FGD-CaSO3可以显着抑制小麦的生长以及碱性磷酸酶和芳基硫酸酯酶的活性。我们得出的结论是,FGD-CaSO3的表面施用可能与石膏一样有效,可抑制土壤结皮,改善水的渗透并促进Ca2 +迁移到酸性土壤中。此外,等于或小于4.4 Mg ha-1的施用量对土壤微生物活动或植物生长没有负面影响。

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