首页> 外文期刊>Soil Science Society of America Journal >Prescribed Fire Alters the Impact of Wildfire on Soil Biochemical Properties in a Ponderosa Pine Forest
【24h】

Prescribed Fire Alters the Impact of Wildfire on Soil Biochemical Properties in a Ponderosa Pine Forest

机译:规定的火灾改变了野火对美国黄松林中土壤生化特性的影响

获取原文
获取原文并翻译 | 示例
       

摘要

Although studies have addressed the influence of fire on soil biochemical processes, there have been no reports on how prescribed fire followed by wildfire influences microbial activity and nutrient cycling. Over a 21-mo period we monitored changes in soil nitrogen (N) and carbon (C) of a ponderosa pine (Pinus ponderosa P.&C. Lawson) and Douglas-fir [Pseudotsuga menziesii var. glauca (Beissn.) Franco] forest (both O horizon and 0–10 cm of mineral soil) that had been exposed either to prescribed fire (PB), wildfire (WF), prescribed fire three months prior to wildfire (PBWF), or no fire as an unburned control. Total N, potentially mineralizable N (PMN), NH+4–N and NO-3–N concentrations in surface (0–10 cm) mineral soils were significantly increased immediately after WF. Soils exposed to prescribed fire prior to wildfire also had elevated concentrations of total N, PMN and NH+4–N, but were significantly lower than in WF alone. Potentially mineralizable N was significantly reduced on all fire-exposed sites from 9 mo to the end of the study period. Although mineral soil NO-3–N concentrations in fire-exposed soils were similar to the unburned control 12 mo after fire, resin sorbed NO-3–N was 88 µg capsule-1 in WF soils vs. 24 µg capsule-1 in PBWF soils, and 1.3 µg capsule-1 in the unburned control. Microbial biomass in the WF mineral soils was as low as 52 µg g-1 21 mo after fire while microbial biomass in PBWF soils remained above 100 µg g-1 throughout the study. It appears that prescribed fire prior to wildfire may attenuate the effects of wildfire on soil and may have predisposed the microbial community to the effects of heating.
机译:尽管研究已经解决了火对土壤 生化过程的影响,但是还没有关于开火后野火如何影响微生物活性和 的报道。营养循环。在21个月的时间内,我们监测了美国黄松(Pinus ponderosa P.&C。Lawson)和道格拉斯-松的土壤氮(N)和碳(C)的变化。冷杉[Pseudotsuga menziesii var。 glauca(Beissn。Franco)森林(O地平线和0–10 cm的矿物土壤)都暴露于规定的 火(PB),野火(WF ),在 野火(PBWF)之前三个月开具明火,或者作为不燃烧的对照不开火。总 N,可能矿化的N(PMN),NH + 4 –N和NO - 3 WF后,表层(0–10 cm)矿质土壤中的 –N 浓度 显着增加。在野火之前暴露于 规定火的土壤中,总N,PMN和NH + 4 的总浓度 – N,但明显低于 。从9 mo到 研究期末,所有受火暴露地点的潜在可矿化N均显着降低。尽管暴露在火中的土壤中矿质土壤NO - 3 –N浓度 与未燃烧对照12 mo相似火灾后,在WF土壤中树脂吸附的NO - 3 –N为88 µg胶囊 -1 ,而24 PBWF土壤中的µg胶囊 -1 和未燃烧对照中的1.3 µg胶囊 -1 。火灾后,WF矿物土壤中的微生物生物量 低至52 µg g -1 21 mo ,而PBWF土壤中的微生物生物量仍高于<在整个研究过程中,sup> 100 µg g -1 。看来在野火之前先开处方的 火可能会减弱野火 对土壤的影响,并且可能使微生物群落更容易受到加热的影响。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号