Li Zhi-an, Zou Bi, Xia Han-ping, Ding Yong-zhen, Tan Wan-neng, Ma Zhen-rong
South China Botanical Garden, Chinese Academy of Sciences, Guangzhou 510650, China.
J Environ Sci (China). 2005;17(6):970-6.
The effects of fertilizers and water content on N2O emission were studied using the three most typical plantation soils. Soil incubations were performed and fertilization and water content treatments were designed. At 25% of saturated water content(SWC), N2O emissions from the soil treated with urea, KNO3, (NH4)2 SO4 and KH2 PO4 were compared at application rates of 0, 100, 200, 300 and 500 kg/hm2. At 80% of SWC, similar experiments were carried out but at only one application rate(500 kg/hm2). N2O emissions at various water contents(20%, 35%, 50%, 65%, 80% and 100% of SWC) were studied. At low water content(25% of SWC), neither nitrogen nor phosphorus(or potassium) fertilizers led to a high level of N2O emission, which generally ranged from 2.03 to 29.02 microg/(m2 x h). However, at high water content(80% SWC), the fertilizers resulted in much greater N2O emission irregardless of soil tested. The highest N2O emission rates after 24 h of water addition were 1233 microg/(m2 x h) for S. superba soil, 1507 microg/(m2 x h) for P. elliottii soil and 1869 microg/ (m2 x h) for A. mangium soil respectively. N2O emission from soils treated with urea, (NH4)2 SO4 and KH2 PO4 immediately dropped to a low level but steadily increased to a very high level for the soil treated with KNO3. High NO3- content was a basis of high level of N2O emission. N2O emission rates from soils peaked shortly after flooding, rapidly dropping to a very low level in soil from non-legume plantations, but lasting for a relatively long period in soil from legume plantations. When soil water content increased equaling to or higher than 65%, the accumulated N2O emission over a period of 13 d ranged from 20.21-29.78 mg/m2 for S. superba, 30.57-70.12 mg/m2 for P. elliottii and 300.89-430.51 mg/m2 for A. mangium. The critical water content was 50% of SWC, above which a high level of N2O emission could be expected, and below which very little N2O emissions were detected. The results suggest that, at low water content (< 50% of SWC), the fertilization practice is safe with regard to N2O emissions, but at high water content (> 50% of SWC), nitrogen fertilizer in the form of nitrate could yield a 100-fold increase in N2O emissions. Legume plantations like A. mangium should be avoided in low lands which could easily suffer from flooding or poor drainage.
利用三种最典型的人工林土壤,研究了肥料和含水量对一氧化二氮(N2O)排放的影响。进行了土壤培养试验,并设计了施肥和含水量处理。在饱和含水量(SWC)的25%时,比较了在施用量为0、100、200、300和500 kg/hm2的情况下,用尿素、硝酸钾、硫酸铵和磷酸二氢钾处理的土壤中N2O的排放情况。在SWC的80%时,进行了类似的试验,但仅采用一个施用量(500 kg/hm2)。研究了不同含水量(SWC的20%、35%、50%、65%、80%和100%)下的N2O排放情况。在低含水量(SWC的25%)时,氮肥和磷肥(或钾肥)均未导致高水平的N2O排放,其排放水平一般在2.03至29.02微克/(平方米·小时)之间。然而,在高含水量(SWC的80%)时,无论测试何种土壤,肥料都会导致更高的N2O排放。加水24小时后,木荷土壤的最高N2O排放率为1233微克/(平方米·小时),湿地松土壤为1507微克/(平方米·小时),马占相思土壤为1869微克/(平方米·小时)。用尿素、硫酸铵和磷酸二氢钾处理的土壤中N2O排放立即降至低水平,但用硝酸钾处理的土壤中N2O排放稳步增加至非常高的水平。高硝酸盐含量是高水平N2O排放的一个基础。淹水后不久,土壤中的N2O排放率达到峰值,非豆科人工林土壤中的N2O排放迅速降至非常低的水平,但豆科人工林土壤中的N2O排放持续较长时间。当土壤含水量增加到等于或高于65%时,13天内木荷土壤累积N2O排放量为每平方米20.21 - 29.78毫克,湿地松土壤为30.57 - 70.12毫克,马占相思土壤为300.89 - 430.51毫克。临界含水量为SWC的50%,高于此值可预期高水平的N2O排放,低于此值则检测到极少的N2O排放。结果表明,在低含水量(<SWC的50%)时,施肥做法在N2O排放方面是安全的,但在高含水量(>SWC的50%)时,硝酸盐形式的氮肥可使N2O排放量增加100倍。在容易遭受洪水或排水不良的低地,应避免种植像马占相思这样的豆科人工林。