首页> 外文期刊>Forest Ecology and Management >Neotropical savanna converted to food cropping and cattle feeding systems: soil carbon and nitrogen changes over 30 years [Review]
【24h】

Neotropical savanna converted to food cropping and cattle feeding systems: soil carbon and nitrogen changes over 30 years [Review]

机译:新热带稀树草原转化为粮食作物和牛饲养系统:30年来土壤碳和氮的变化[综述]

获取原文
获取原文并翻译 | 示例
           

摘要

This work analyzed the effects of management practices over 30 years in Orinoco savanna ultisols. The long-term effects were evaluated by comparing soil organic carbon (SOC) and total nitrogen (TN) changes, as well as carbon and nitrogen mineralization, in (1) a continuous woodland-savanna fallow (T1); (2) a perennial Brachiaria (Brachiaria decumbens Stapf.) field under intensive cattle raising (T2), which was tilled and renewed every 5 years; (3) a cowpea (Vigna unguiculata (L.) Walp.) field (T3), which was annually tilled and fallowed during the rest of the year; and (4) native savanna under extensive cattle raising (T4). Management practices (i.e. T2-T4) corresponded to the productive systems under conditions representative of normal use in the Orinoco llanos. The fallow influenced the quantity and quality (i.e. mineralizable C and N) of soil organic matter. Over 30 years, the effect of savanna fallow was to increase the SOC and TN from 2092 +/- 295 and 153 +/- 24 to 3514 +/- 300 and 310 +/- 46 g m(-2), respectively. In this fallow treatment, the temporal pattern of SOC and TN changes were described by an exponential increase after 15 years of fallowing. For the grazed Brachiaria, cowpea and native grazing savanna, SOC and TN remained in equilibrium throughout the period. The soil potential N mineralization, in the woodland-savanna fallow, reached 21.4 g N m(-2). In the other treatments, it ranged from 10.0 to 11.8 g N m(-2). In all plots, the NH4-N/NO3-N ratio was above unity and nitrification occurred in the absence of amotrophic nitritiers. Carbon mineralization in the woodland-savanna fallow, as expressed by field measurements of the annual heterotrophic respiration (628 g C m(-2) per year), was lower than that in the other systems. However, microbial density did not differ between treatments. Over 30 years, different SOC and TN levels in the soil treatments were related to litter input production. The described sustainable use of the analyzed systems provided clues for conserving soil and maintaining system productivity in the Orinoco Ilanos and comparable lowlands under similar climatic and edaphic conditions. However, optimal combination of organic and inorganic fertilizers depends on both socio-economic and environmental factors.
机译:这项工作分析了30年来Orinoco稀树草原野生动物管理实践的影响。通过比较(1)连续林地-热带稀树草原(T1)中土壤有机碳(SOC)和总氮(TN)的变化以及碳和氮矿化作用,评估了长期影响。 (2)在集约化养牛(T2)下的多年生Bracharia(Brachiaria decumbens Stapf。)田地,每5年耕种并更新一次; (3)cow豆(Vigna unguiculata(L.)Walp。)田(T3),在该年剩余时间每年进行耕种和休耕; (4)大量养牛(T4)下的本地稀树草原。管理实践(即T2-T4)对应于Orinoco llanos正常使用条件下的生产系统。休耕影响土壤有机质的数量和质量(即可矿化的碳和氮)。在超过30年的时间里,稀树草原的影响是使SOC和TN从2092 +/- 295和153 +/- 24分别增加到3514 +/- 300和310 +/- 46 g m(-2)。在这种休闲疗法中,SOC和TN变化的时间模式通过休闲15年后的指数增加来描述。对于放牧的腕足动物,cow豆和本地放牧大草原,SOC和TN在整个时期内保持平衡。在林地-热带稀树草原休耕地中,土壤潜在的氮矿化量达到21.4 g N m(-2)。在其他处理中,其范围从10.0到11.8 g N m(-2)。在所有地块中,NH4-N / NO3-N的比率均大于1,并且在不存在营养缺陷型硝化剂的情况下发生硝化作用。林地-热带稀树草原休耕地的碳矿化,通过年度异养呼吸的实地测量(每年628 g C m(-2))来表示,低于其他系统。但是,不同处理之间的微生物密度没有差异。 30多年来,土壤处理中不同的SOC和TN水平与垫料投入生产相关。所描述的分析系统的可持续利用为在类似的气候和水文条件下的Orinoco Ilanos和类似的低地保护土壤和维持系统生产力提供了线索。但是,有机和无机肥料的最佳组合取决于社会经济和环境因素。

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