1) legal factor
合法因素
2) Element association method
因素组合法
3) Synthetical 3 factors method
综合三因素方法
4) the multifactor comprehensive method
多因素综合法
1.
According to"the soil erosion classification grade criteria"(SL 190-96) issued by the Ministry of Water Resources,the multifactor comprehensive method in the second national soil erosion investigation based on remote sensing was adopted,and land use type,the fractional vegetation cover and slope were the three factors affecting soil erosion.
以北京地区L andsat ETM和DEM为主要数据源,依据水利部颁布的《土壤侵蚀分类分级标准》(SL 190-96),采用了第二次全国土壤侵蚀遥感调查中的多因素综合法,选取土地利用类型、植被覆盖度和坡度三个因子,对北京地区水土流失状况进行了快速监测,该方法简单易行,结果基本符合实际情况。
5) component forcasting method
因素组合预测法
6) single factor analysis and multifactor comprehensive mapping method
单因素分析多因素综合作图法
1.
On the basis of all kinds of stratigraphic and petrologic data of outcrop and well sections,the maps of single factors and sedimentary facies of the Paleocene-Eocene,Oligocene and Miocene were compiled with the single factor analysis and multifactor comprehensive mapping method proposed by Professor Feng Zengzhao.
根据柴达木盆地北缘露头剖面、钻井剖面的地层学和岩石学研究所取得的各种定量及定性资料,采用冯增昭教授倡导的单因素分析多因素综合作图法,编制了柴达木盆地北缘结绿素—红山地区古新统—始新统、渐新统和中新统的各种单因素图和沉积相图。
2.
Based on all kinds of qualitative and quantitative data of stratigraphy and petrology of outcrops and well logs,according to the single factor analysis and multifactor comprehensive mapping method which was proposed by Professor Feng Zengzhao,the maps of single factors and sedimentary facies of the Lower,Middle and Upper Jurassic have been compiled.
在各露头剖面、钻井剖面地层学和岩石学研究所取得的各种定性及定量资料的基础上,采用冯增昭教授倡导的单因素分析多因素综合作图法,编制出了柴达木盆地北缘结绿素—红山地区下、中、上侏罗统的各类单因素图件和沉积相图。
补充资料：非密度制约因素(见密度制约因素)
非密度制约因素(见密度制约因素)
l焦非密度制约因素见生态因素、密度制约后
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条