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Long-term irrigation effects on soil organic matter under temperate grazed pasture

机译:温带草场长期灌溉对土壤有机质的影响

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摘要

Irrigation of grazed pasture significantly increases plant and animal production, which may in turn increase soil organic carbon (SOC), depending on the balance between primary production and below-ground allocation of C on the one hand, and the decomposition and export of C from the soil on the other. To evaluate the effect of irrigation on SOC we sampled a grazed pasture field experiment maintained under different irrigation treatments for 62 years. The dry-land treatment in this experiment only received rainfall at an average of 740 mm year(-1). The 10 and 20% irrigation treatments involved application of 100 mm of irrigation when the soil reached 10 and 20% gravimetric moisture content, respectively. The 10 and 20% irrigation treatments received average total annual irrigation inputs of 260 and 770 mm year(-1), respectively. The 10 and 20% irrigation treatments increased pasture production by 44 and 74%, respectively, compared with that from the dry-land. Analysis of soils taken to 1-m depth revealed that amounts of SOC were not significantly different between the dry-land (125.5 Mg ha(-1)) and 10% irrigation (117.8 Mg ha(-1)) treatments, but these were significantly greater than the 20% irrigation treatment (93.0 Mg ha(-1)). At 50-100 cm, SOC was also less (34%) for the 20% irrigation treatment than for the 10% irrigation treatment. The relative quantities of carbon (C) and nitrogen (N) in the light fraction (LF) at all soil depths decreased successively from dry-land to the 20% irrigation treatment, suggesting that wetter soil conditions accelerated decomposition of the LF fraction, a comparatively labile SOC fraction. The C-to-N ratio of the bulk soil was also less for the 20% irrigation treatment, indicating more decomposed SOM in the irrigated than in the dry-land treatment. There were no significant differences in the microbial biomass between the three different irrigation treatments, but the respiration rate (CO2 production) of soil organisms in the 20% irrigation treatment was consistently greater than in the other two treatments. It was concluded that large increases in plant productivity as a result of irrigation had either no effect or significantly reduced SOC stocks under grazed pasture. The reduced SOC content observed in the 20% irrigation treatment was attributed to a combination of increased C losses in animal products and drainage associated with greater stocking, together with accelerated decomposition of organic C resulting from elevated soil moisture maintained throughout the growing season
机译:放牧牧场的灌溉显着增加了动植物的生产,这可能反过来又增加了土壤有机碳(SOC),这取决于一方面C的初级生产与地下分配之间的平衡,以及C的分解和输出在另一个土壤上。为了评估灌溉对土壤有机碳的影响,我们采样了在不同灌溉条件下维持62年的放牧牧场试验。在本实验中,旱地处理仅接受平均740毫米年(-1)的降雨。 10%和20%的灌溉处理涉及当土壤分别达到10和20%的重量含水量时进行100 mm的灌溉。 10%和20%的灌溉处理平均每年的总灌溉输入分别为260和770 mm年(-1)。与干旱地区相比,灌溉方式的10%和20%可使牧草产量分别增加44%和74%。对深度为1 m的土壤进行的分析表明,旱地(125.5 Mg ha(-1))和10%灌溉(117.8 Mg ha(-1))处理之间的SOC量没有显着差异,但这些明显大于20%的灌溉处理(93.0 Mg ha(-1))。在50-100 cm,20%灌溉处理的SOC也比10%灌溉处理的SOC低(34%)。从干旱地区到20%灌溉处理,所有土壤深度的轻组分(LF)中的碳(C)和氮(N)的相对数量依次减少,这表明潮湿的土壤条件加速了LF组分的分解,相对不稳定的SOC分数。在20%的灌溉条件下,散装土壤的C / N比也较小,这表明灌溉条件下的SOM比干地处理的分解率更高。三种不同灌溉处理之间的微生物量没有显着差异,但是20%灌溉处理中土壤生物的呼吸速率(CO2产生)始终高于其他两种处理。得出的结论是,灌溉带来的植物生产力的大幅度提高对草食牧场下的SOC储量没有影响或没有明显减少。在20%的灌溉处理中观察到的SOC含量降低是由于动物产品中的C损失增加和放牧导致的排水增加,以及整个生长季节保持的土壤湿度升高导致有机C分解加速所致。

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