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Influence of soil and water conservation measures on soil fertility in the Beijing mountain area

机译:水土保持措施对北京山区土壤肥力的影响

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摘要

Soil and water conservation (SWC) measures can be adopted to conserve soil and water and improve soil fertility. The degree to which SWC measures improve soil fertility is affected by the type of SWC measure, soil type, climate, etc. The purpose of this study was to study the effect of the main SWC measures implemented in the Beijing mountain area on soil fertility. Six runoff plots, including a fish pit (fallow) (FPF), fish pit (Platycladus orientalis L. Franco) (FPP), narrow terrace (fallow) (NTF), narrow terrace (Juglans regia L.) (NTJ), tree pan (Juglans regia L.) (TPJ), and fallow land (FL), were established to analyze the differences in soil fertility in the Beijing mountain area. Soil samples were collected in 2005 and 2015 from the six runoff plots. Soil particle size; soil total nitrogen (TN), total phosphorous (TP), total potassium (TK), alkali-hydrolysable nitrogen (Ah-N), available P (Av-P), and available K (Av-K); and soil organic matter (SOM) were measured. The soil integrated fertility index (IFI) was calculated. The results showed that the soil nutrient content and IFI significantly decreased from 2005 to 2015 in the FL plot and significantly increased in the five runoff plots with SWC measures. Compared to the other runoff plots with SWC measures, the FPP plot more significantly improved the soil nutrient content and IFI. The TN, Ah-N, Av-K, SOM, and IFI in the FPP plots increased by 98%, 113%, 61%, 69 and 47%, respectively, from 2005 to 2015. The IFI for the FPP, NTJ, and TPJ exceeded the average IFI of the farmland soil in the study region. The results indicated that the combination of engineering practices and vegetative measures effectively improved soil fertility. These results may be helpful for selecting SWC measures, land-use planning and monitoring and assessing soil fertility.
机译:可以采取水土保持措施来保护水土和提高土壤肥力。 SWC措施提高土壤肥力的程度受SWC措施类型,土壤类型,气候等因素的影响。本研究的目的是研究北京山区实施的主要SWC措施对土壤肥力的影响。六个径流地块,包括鱼池(休耕区)(FPF),鱼池(侧柏(Platycladus Orientalis L. Franco)(FPP),狭窄梯田(休耕)(NTF),狭窄梯田(胡桃兰)(NTJ),树建立了Pan(Juglans regia L.)(TPJ)和休耕地(FL)来分析北京山区土壤肥力的差异。 2005年和2015年从六个径流地块收集了土壤样品。土壤粒径;土壤总氮(TN),总磷(TP),总钾(TK),碱解氮(Ah-N),有效磷(Av-P)和有效钾(Av-K);测定土壤有机质(SOM)。计算了土壤综合肥力指数(IFI)。结果表明,从2005年到2015年,FL样地的土壤养分含量和IFI显着下降,而采用SWC措施的五个径流样地中的土壤养分含量和IFI则显着增加。与采用SWC措施的其他径流图相比,FPP图更明显地改善了土壤养分含量和IFI。从2005年到2015年,FPP地块中的TN,Ah-N,Av-K,SOM和IFI分别增长了98%,113%,61%,69和47%。FPP,NTJ, TPJ超过研究区域农田土壤的平均IFI。结果表明,将工程实践与营养措施相结合可以有效地提高土壤肥力。这些结果可能有助于选择SWC措施,土地利用规划以及监测和评估土壤肥力。

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