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Effect of long-term N fertilization on ca saturation and soil quality in a calcareous soil in a semiarid to sub-humid region

机译:半干旱半湿润地区石灰性土壤长期施氮对钙饱和度和土壤质量的影响

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This objective of this study was to investigate the effect of long-term N fertilizer application on Calcium (Ca) saturation in a calcareous farmland soil located in a semiarid to subhumid region. The soil type was a Lou soil (Eum-Orthic Anthrosol). Results from this study provide important information about the relationship between fertilization and soil fatigue in farmland. The study also provides insight about soil factors that impact crop stress resistance and changes traditional concepts regarding the Ca balance in calcareous soils. The results showed that across the landscape there was moderate variation in the soil organic matter content of the 10 to 20 cm soil layer. The soil organic matter content was highest near to the village, reflecting the traditional use of organic manure on the Guanzhong Plain and confirming the principle of “village at the center”. This result also highlighted uneven soil quality across the landscape due to human activity. The soil organic matter content was less but the soil available N content was greater in the 0 to 10 cm layer than the 10 to 20 cm layer. This observation is probably due to the application of inorganic fertilizer in modern agriculture. Soil Ca saturation declined by 15.38 to 14.46% as the distance from the village increased. This observation is probably due to interaction between ancient and modern fertilization practices as well as recent land policies. The pattern of changes for soil Ca saturation across the landscape was similar to the pattern of changes for soil organic matter content but opposite to the pattern of changes for soil available N. This proved that application of large amounts of inorganic N fertilizer can increase inorganic soil N and decrease Ca saturation. This is one symptom of soil potential degradation or soil fatigue. In summary, the application of inorganic fertilizer resulted in a significant decrease in the percent of soil Ca saturation in this calcareous soil. This indicates that the application of inorganic N fertilizer can cause a considerable decline in soil health and reduce the effectiveness of modern fertilizers.
机译:这项研究的目的是调查长期施用氮肥对半干旱至半湿润地区钙质农田土壤钙(Ca)饱和度的影响。土壤类型为娄土(欧姆-正统人烟)。这项研究的结果提供了有关施肥与农田土壤疲劳之间关系的重要信息。这项研究还提供了有关影响作物抗逆性的土壤因素的见解,并改变了钙质土壤中钙平衡的传统观念。结果表明,在整个景观中,10至20 cm土层的土壤有机质含量变化适中。该村附近的土壤有机质含量最高,这反映了关中平原地区传统有机肥的使用,并印证了“以村庄为中心”的原则。该结果还突出了由于人类活动造成的整个景观土壤质量不均。土壤有机质含量较低,但0至10 cm层的土壤有效氮含量高于10至20 cm层。这种观察可能是由于无机肥料在现代农业中的应用。随着距村庄的距离增加,土壤钙饱和度下降了15.38%至14.46%。这种观察可能是由于古代和现代的施肥方式以及最近的土地政策之间的相互作用。整个景观区土壤钙饱和度的变化规律与土壤有机质含量的变化规律相似,但与土壤有效氮的变化规律相反。这证明了施用大量无机氮肥可以增加无机土壤的含量。 N和降低Ca饱和度。这是土壤潜在退化或土壤疲劳的一种症状。总而言之,无机肥料的施用导致了钙质土壤中钙饱和度的百分比显着降低。这表明无机氮肥的施用会导致土壤健康显着下降,并降低现代肥料的有效性。

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