;where i is number of soil layer; – average density of soil composition as per soil profile, t/m3; to determine average profile values of MMC % of MSP: a) when measurements are taken on layers of equal power: , b) when conducting the horizontal measurements (WMMC)i with different thickness of genetic horizons by relationship of the form: , where j is the depth of the profile in question, m; n is the number of soil layers of equal power; hhor A, hhor B1, hhor B2, hhor Bs – thickness of genetic horizons A, B1, B2 and Bs within the considered meter-long soil profile, m; c) at known average or averaged values by: .;EFFECT: method makes it possible to simplify determination of minimum moisture capacity of soil in field conditions due to analytical method of determination.;1 cl, 2 tbl"/> EXPERIMENTAL-ANALYTICAL METHOD FOR DETERMINING MINIMUM MOISTURE CAPACITY OF CHERNOZEMS AND CHESTNUT SOILS
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EXPERIMENTAL-ANALYTICAL METHOD FOR DETERMINING MINIMUM MOISTURE CAPACITY OF CHERNOZEMS AND CHESTNUT SOILS

机译:测定菜豆和栗子土壤最小水分容量的实验分析方法

摘要

FIELD: ecology.;SUBSTANCE: invention relates to the field of land reclamation. In method of determining minimum moisture capacity (MMC) of chernozem and chestnut soils of steppe and dry steppe types of soil formation, analytical determination of minimum moisture capacity of soil is determined – a complexly determined soil parameter according to experimentally established soil characteristics – values of content in soil of physical clay ((Wc)i, % MSP) and humus ((ghum)i, %), density of soil (γi, t/m3) and thickness of humus horizon (hhum, m) using relationships: for determining soil MMC values (WMMC)i, % MSP: ; ;where i is number of soil layer; – average density of soil composition as per soil profile, t/m3; to determine average profile values of MMC % of MSP: a) when measurements are taken on layers of equal power: , b) when conducting the horizontal measurements (WMMC)i with different thickness of genetic horizons by relationship of the form: , where j is the depth of the profile in question, m; n is the number of soil layers of equal power; hhor A, hhor B1, hhor B2, hhor Bs – thickness of genetic horizons A, B1, B2 and Bs within the considered meter-long soil profile, m; c) at known average or averaged values by: .;EFFECT: method makes it possible to simplify determination of minimum moisture capacity of soil in field conditions due to analytical method of determination.;1 cl, 2 tbl
机译:技术领域本发明涉及土地开垦领域。在确定干草原和干草原类型的黑钙土和栗子土壤的最小水分容忍度(MMC)的方法中,确定土壤的最小水分容忍度的分析确定–根据实验确定的土壤特性综合确定的土壤参数–土壤中的黏土含量((W c i ,%MSP)和腐殖质((g hum i ,%),土壤密度(γ i ,t / m 3 )和腐殖质层厚度(h hum ,m)使用关系:用于确定土壤MMC值(W MMC i ,%MSP: ; i是土层数; –根据土壤剖面的土壤成分平均密度,t / m 3 < / Sup>;确定MMC的平均配置文件值<图像文件=“ 00000032.JPG” he =“ 8” imgContent =“ undefined” imgFormat =“ JPEG” wi =“ 17” /> MSP的百分比:a)在图层上进行测量时相等的功率:,b)进行水平测量时(W MMC < / Sub>) i ,通过以下形式的关系具有不同的遗传层次:,其中j是所讨论轮廓的深度,m; n是相等功率的土壤层数; h hor A ,h hor B1 ,h hor B2 ,h hor Bs –遗传水平A的厚度,在考虑的米长土壤剖面m内的B 1 ,B 2 和B s c)以已知的平均值或平均值<图像文件=“ 00000035.JPG” he =“ 8” imgContent =“ undefined” imgFormat =“ JPEG” wi =“ 28” />通过:<图像文件=“ 00000036.JPG” heff; 9“ imgContent =” undefined“ imgFormat =” JPEG“ wi =” 155“ />。;效果:由于分析方法的确定,该方法可以简化田间条件下土壤最小水分容量的确定。 1厘升,2汤匙

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