中文摘要：

应用文献学方法、野外勘查和实测数据，研究六百年来汾河上游行政区划变迁、人口、耕地和土壤侵蚀的发展，得到以下结论：（1）本区耕地增长远不及人口增长，故人均耕地减少1／3，而粮食单产并无明显提高；（2）通过对晚清阳曲县府推行土地清丈的成果分析，指出当时官方公布的耕地数不及实际数的一半；（3）清乾隆至光绪间，因坡地开垦而使侵蚀量有所增加，但在总侵蚀量中比重极小；（4）清光绪朝至今，由于较多开垦陡、急坡地，人为因素有所增长，但耕地上的侵蚀仍远少于自然力导致的沟蚀，只居次要地位。

英文摘要：

The aim of this study is mainly to deal with the impact of human farming activities on the environmental changes especially the soil erosion in the upper reaches of the Fenhe River in recent 600 years. Through field investigation and the analysis of the longterm data of hydrology and landscape, the authors used the historical documentation method to make a quantitative analysis and estimate farming population, farmland and soil erosion development process of the study area. The study indicates that： （1）In recent 600 years, the population of the area increased by 716%, while the farmland merely 432 %. So the farmland per capita available decreased by 34.8 %. At the same time, per mu （15mu=1ha） average corn yield mu was only about 50kg lower than that in the middle reaches of the Yellow River in the Han Dynasty. The trend of reclamation still exited. （2）Through the analysis of the result of land measurement of Yangqu county in later Qing Dynasty, we thought the data of farmland area were far less from the actual amount, which was possiblely less than the half. （3） From the Qianlong to the Guangxu years of the Qing Dynasty, soil erosion amount increased because of slope farming, which was only 2% - 3% of the total eroded amount and cannot play the dominant role. （4）From the Guangxu years of the Qing Dynasty to modern times, much scarp and steep slope land was reclaimed in the Fenhe river basin which led to the soil erosion increased to 30 % of the total amount. But the amount of the gully erosion induced by natural force was also 70 %. So the farming activity was merely the second factor for the soil erosion.