首页> 外文期刊>European Journal of Soil Science >Organic carbon additions: effects on soil bio-physical and physico-chemical properties
【24h】

Organic carbon additions: effects on soil bio-physical and physico-chemical properties

机译:添加有机碳:对土壤生物物理和物理化学特性的影响

获取原文
获取原文并翻译 | 示例
           

摘要

The effects of organic carbon (OC) additions from farm manures and crop residues on selected soil bio-physical and physico-chemical properties were measured at seven experimental sites, on contrasting soil types, with a history of repeated applications of farm manure or differential rates of inorganic fertilizer nitrogen (N). Repeated (> 7 years annual additions) and relatively large OC inputs (up to 65 t OC ha(-1)) were needed to produce measurable changes in soil properties, particularly physical properties. However, over all the study sites, there was a positive relationship between OC inputs and changes in total soil OC and 'light' fraction OC (LFOC), with LFOC providing a more sensitive indicator of changes in soil organic matter status. Total soil OC increased by an average of 3% for every 10 t ha(-1) manure OC applied, whereas LFOC increased by c. 14%. The measured soil OC increases were equivalent to c. 23% of the manure OC applied (up to 65 t OC ha(-1) applied over 9 years) and c. 22% of the crop residue OC applied (up to 32 t OC ha(-1) over 23 years). The manure OC inputs (but not crop residue OC inputs) increased topsoil porosity and plant available water capacity, and decreased bulk density by 0.6%, 2.5% and 0.5% with every 10 t ha(-1) manure OC applied, respectively. Both OC sources increased the size of the microbial biomass (11% increase in biomass C with 10 t OC ha(-1) input), but only manure OC increased its activity (16% increase in the soil respiration rate with 10 t OC ha(-1) input). Likewise, the potentially mineralizable N pool only increased with manure N inputs (14% increase with 1 t manure total N ha(-1)). However, these soil quality benefits need to be balanced with any potential environmental impacts, such as excessive nutrient accumulation, increased nitrate leaching and phosphorus losses and gaseous emissions to the atmosphere.
机译:在七个不同的土壤实验地点,测量了农场粪便和农作物残留物中有机碳(OC)对选定的土壤生物物理和理化特性的影响,并具有重复施用农场粪便或不同比率的历史。无机肥料中的氮(N)。为了产生可测量的土壤特性(尤其是物理特性)变化,需要重复(每年增加7年以上)和相对较大的OC输入(最大65 t OC ha(-1))。但是,在所有研究地点中,OC输入与总土壤OC和“轻度”分数OC(LFOC)的变化之间存在正相关,而LFOC提供了更敏感的土壤有机质状态变化指标。每施用10 t ha(-1)肥料,总土壤OC平均增加3%,而LFOC增加c。 14%。测得的土壤OC增量等于c。施用了23%的肥料OC(在9年内施用了65 t OC ha(-1))和c。施用了22%的农作物残余OC(在23年中高达32 t OC ha(-1))。每施用10 t ha(-1)粪肥OC,粪肥OC的输入量(而不是农作物残余物OC的输入量)增加了表土孔隙度和植物的可用水容量,并使堆积密度分别降低了0.6%,2.5%和0.5%。两种OC来源都增加了微生物生物量的大小(输入10吨OC ha(-1)时生物量C增加11%),但只有粪肥OC才增加其活性(10吨OC ha时土壤呼吸速率增加16%)。 (-1)输入)。同样,潜在可矿化的氮库仅随着粪肥氮输入量的增加而增加(粪肥总氮素ha(-1)增加1吨时增加14%)。但是,这些土壤质量的好处需要与任何潜在的环境影响相平衡,例如过多的养分积累,增加的硝酸盐浸出和磷的损失以及向大气中的气体排放。

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