• ISSN 1008-505X
  • CN 11-3996/S

氮肥形态及用量对坡耕地红壤pH的影响机理

Mechanisms of nitrogen fertilizer types and rates on pH of red soil in sloping farmland

  • 摘要:
    目的 硝化释放氢离子(H+)是化学氮肥加速农田红壤酸化的主要过程之一。坡耕地红壤以“酸、瘦”为基本特征且硝化能力弱,厘清不同形态氮肥对坡耕地红壤pH的影响特征,为红壤区坡耕地酸化防治提供理论依据。
    方法 开展化肥形态和尿素用量两个玉米盆栽试验,供试土壤为坡耕地红壤。化肥形态试验设6个氮肥形态处理:尿素、硫酸铵、硝酸铵、碳酸铵、氯化铵、硝酸钾,施氮量均为N 200 mg/(kg,土);尿素用量试验设置施N 25 mg/kg (N25)、50 mg/kg (N50)、100 mg/kg (N100)、200 mg/kg (N200)、300 mg/kg (N300)、400 mg/kg (N400);两个试验均以不施肥 (CK1)和只施磷钾肥 (CK2)为对照。玉米播种后45天收获,玉米植株样品测定植株生物量及养分含量,土壤样品测定pH、盐基离子、无机氮含量。
    结果 与CK1、CK2相比,除尿素外的5个氮肥形态处理土壤pH均显著降低,以硫酸铵和氯化铵处理的降幅最大,为0.74~0.87个单位,其次为硝酸铵、碳酸铵和硝酸钾处理,降幅为0.34~0.37个单位,而尿素处理与CK1无显著差异,但显著高于CK2。当尿素N施用量<200 mg/kg时,土壤pH与CK1无显著差异,但显著高于CK2;施N量为300 mg/kg时,pH与CK2相当但显著低于CK1,而施N量为400 mg/kg时,pH显著低于CK1和CK2 (P<0.05)。与CK1和CK2相比,硫酸铵、硝酸铵、碳酸铵和硝酸钾处理土壤交换性钙、镁离子含量分别降低了0.89~1.74和0.19~0.30 cmol/kg;与CK1相比,尿素N50~N400 处理分别降低了0.43~0.81和0.11~0.25 cmol/kg;与CK1、CK2相比,除硝酸钾处理交换性钾离子显著增加外,其余处理交换性钾、钠离子含量无显著变化。与CK1相比,硫酸铵、碳酸铵以及尿素N300和N400处理土壤铵态氮含量增加了18.45~119.36 mg/kg,硝酸铵、硝酸钾以及尿素N300和N400处理土壤硝态氮含量增加了7.26~50.09 mg/kg;与CK2相比,尿素、硫酸铵、碳酸铵以及尿素N300、N400处理土壤铵态氮含量显著增加了16.17~123.60 mg/kg,硝酸铵、硝酸钾以及尿素N300、N400处理土壤硝态氮显著增加了6.40~49.23 mg/kg。与CK1和CK2相比,除硝酸钾处理玉米茎叶镁含量外,各氮肥形态处理玉米茎叶镁含量显著增加,根钙含量均显著增加,且玉米茎叶和根的钙、镁含量均随尿素N施用量的增加而增加。土壤pH与土壤交换性钙、镁呈显著或极显著正相关,与玉米氮、磷、钙、镁、钾吸收量均呈极显著负相关,与玉米钠吸收量呈显著负相关。
    结论 在红壤坡耕地上,施用硫酸铵和氯化铵对土壤pH的降低幅度最大,其次为碳酸铵、硝酸铵和硝酸钾,而施用适量尿素不会降低土壤pH。硫酸铵、氯化铵、碳酸铵和硝酸铵主要通过硝化释放氢离子降低土壤pH,而尿素和硝酸钾主要通过促进盐基离子吸收产酸。因此,该贫瘠坡耕地红壤复耕前期化学氮肥施用应以尿素为主。

     

    Abstract:
    Objectives The releases of hydrogen ions (H+) during nitrification is one of the main reason of nitrogen fertilizer accelerating the acidification of red soils. Sloping cropland derived of red soil are characterized by acidity and infertility with low nitrification capacity. We studied the acidification effect of nitrogen fertilizers to provide a theoretical basis for alleviation of soil acidification in red soil areas.
    Methods Two maize pot experiments were conducted, one examined the effects of urea, ammonium sulfate (AS), ammonium nitrate (AN), ammonium carbonate (AC), ammonium chloride (ACl), potassium nitrate (PN) under the same N application rate of 200 mg/(kg, soil). The other experiment investigated the effects of urea N doses (25, 50, 100, 200, 300, 400 mg/kg). No fertilization (CK1) and only phosphorus and potassium fertilization (CK2) were used as the controls of the two experiments. The maize plants were harvested 45 days after sowing and plant biomass and nutrient content were determined, and soil samples were analyzed for pH, basic ions, and inorganic nitrogen content.
    Results Compared to CK1 and CK2, all the nitrogen fertilizers except urea decreased soil pH (P<0.05). AS and ACl lowered the pH by 0.74 to 0.87 units, and AN, AC, and KN lowered pH by 0.34 to 0.37 units. The urea-N did not decrease soil pH until the N rate reaching 400 mg/kg. Compared to CK1 and CK2, AS, AN, AC, and KN decreased soil exchangeable Ca by 0.89–1.74 cmol/kg and exchangeable Mg by 0.19–0.30 cmol/kg, with the decrement in descent order of AS, AN, AC and KN. The urea N50–N400 treatments reduced exchangeable Ca by 0.21–0.46 cmol/kg and exchangeable Mg by 0.11–0.25 cmol/kg, respectively. Fertilizer types and urea-N dosages did not affect exchangeable K and Na significantly. Compared to CK1 and CK2, the AS, AC, and urea N 300 and N400 treatments (P<0.05) increased soil NH4+-N by 18.45–119.36 mg/kg and 16.17–123.60 mg/kg, the AN, KN, and urea-N 300 and 400 treatments (P<0.05) increased the NO3--N by 16.83–50.09 mg/kg and 15.97–49.23 mg/kg. All the N fertilizer treatments (P<0.05) increased Ca content in maize shoots and Mg in roots. The Ca and Mg content in maize shoot and root increased with the enhanced urea N rate. Soil pH was (P<0.05) positively correlated with soil exchangeable Ca and Mg content, negatively (P<0.01) correlated with maize N, P, Ca, Mg, and K uptake, and negatively (P<0.05) correlated with maize Na uptake.
    Conclusions In sloping croplands derived of red soils, the most pronounced pH decrease was by application of ammonium sulfate and ammonium chloride, followed by ammonium bicarbonate, ammonium nitrate, and potassium nitrate. Appropriate urea rate would not lower the soil pH. Ammonium sulfate, ammonium chloride, ammonium bicarbonate, and ammonium nitrate primarily reduced soil pH by releasing hydrogen ions through nitrification, while urea and potassium nitrate primarily promoted acid production through the absorption of base ions. Therefore, urea is recommended as nitrogen fertilizers in the early stages of re-cultivation of infertile sloping cultivated red soils.

     

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