中国不同地理区域农业产量生产能量流评价与能源经济分析

Kai Li
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摘要

干燥和潮湿气候对土壤水分的提供具有不同的潜力。农业干旱是评价农业生产潜力的公认标准,本文对此进行了探讨。因此,本研究旨在利用气象和农业干旱指标数据对中国4个气候区(湿润、半湿润、半干旱和干燥)进行干旱调查。为此,收集了近20 a的气候资料,确定了标准降水指数(SPI)和侦察干旱指数(RDI)的数值。对指标的审查表明,在审查的所有年份中,干旱地区的指标都很高。在半干旱区,2017-2022年7月和8月的指数平均值明显下降。湿润和半湿润地区干旱指标不严重,全年植物水分充足。结果表明,在所有鉴定的地区,SPI与RDI之间存在较高的相关性。除降雨外,RDI还包括蒸腾,并且更敏感,特别是在蒸腾高于降雨量的干燥地区。
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Evaluation energy flow and analysis of energy economy for agricultural yield production in different geographical regions of China
Abstract Dry and humid climates have different potentials for providing soil moisture. Agricultural drought is a confirmed criterion for evaluating production potential in agriculture, which is discussed in this research. Therefore, this research aims to investigate drought using meteorological and agricultural drought indicator data in four climatic regions of China (humid, semi-humid, semi-arid and dry). For this purpose, climatic information was collected in the last 20 years, and the values of the standard precipitation index (SPI) and reconnaissance drought index (RDI) were determined. Examining the indicators indicates that the indicators are high in all the years under review in dry areas. In the semi-arid region, there was a significant decrease in the average value of the indices in July and August in the years 2017–2022. Drought indicators did not show a critical situation in humid and semi-humid areas, and there was sufficient moisture for plants throughout the year. The results showed that there was a high correlation between the SPI and the RDI in all the identified areas. In addition to rainfall, the RDI also includes transpiration and is more sensitive, especially in dry areas where transpiration is higher than rainfall.
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