人民黄河
人民黃河
인민황하
Yellow River
2014年
12期
140-142
,共3页
盐渍化%地下水埋深%矿化度%沙坡头灌区
鹽漬化%地下水埋深%礦化度%沙坡頭灌區
염지화%지하수매심%광화도%사파두관구
salinization%groundwater depth%salinity%Shapotou irrigated area
基于宁夏第五次土壤盐渍化调查数据,以宁夏沙坡头灌区为对象,分析高位灌区对低位灌区土壤盐渍化的影响,系统阐述地下水埋深、矿化度与土壤盐渍化的关系,得出:①南山台子扬水灌区对低位灌区的影响范围为350~550m,由高位灌区前沿向低位灌区延伸,土壤盐渍化程度由重变轻;②根据地下水埋深与土壤盐化模型分析结果,春灌前地下水埋深越小,土壤盐分积累越快,含盐量越大;③地下水矿化度的大小影响土壤盐渍化的程度,矿化度越大,土壤盐渍化程度越重。
基于寧夏第五次土壤鹽漬化調查數據,以寧夏沙坡頭灌區為對象,分析高位灌區對低位灌區土壤鹽漬化的影響,繫統闡述地下水埋深、礦化度與土壤鹽漬化的關繫,得齣:①南山檯子颺水灌區對低位灌區的影響範圍為350~550m,由高位灌區前沿嚮低位灌區延伸,土壤鹽漬化程度由重變輕;②根據地下水埋深與土壤鹽化模型分析結果,春灌前地下水埋深越小,土壤鹽分積纍越快,含鹽量越大;③地下水礦化度的大小影響土壤鹽漬化的程度,礦化度越大,土壤鹽漬化程度越重。
기우저하제오차토양염지화조사수거,이저하사파두관구위대상,분석고위관구대저위관구토양염지화적영향,계통천술지하수매심、광화도여토양염지화적관계,득출:①남산태자양수관구대저위관구적영향범위위350~550m,유고위관구전연향저위관구연신,토양염지화정도유중변경;②근거지하수매심여토양염화모형분석결과,춘관전지하수매심월소,토양염분적루월쾌,함염량월대;③지하수광화도적대소영향토양염지화적정도,광화도월대,토양염지화정도월중。
Based on the data of soil salinization investigation in Ningxia Province and taking Shapotou irrigation area as an object,the paper ana-lyzed the influence of salinization of higher elevation irrigation area to the lower elevation irrigation area and discussed the relationship between sa-linity,depth of groundwater and soil salinization. The conclusions are that a)the Nanshantaizi pumping irrigation area impacts the low irrigation ar-ea,the range is 350 ~ 550 m,from high to low irrigation area extending direction,the soil salinization from heavy to light. b)As the result of model,before the spring irrigation,the shallower the groundwater depth is,the faster the soil salt accumulation and higher the salt content will be. c)The groundwater salinity affects the degree of soil salinization. The higher the salinity is,the more serious soil salinization will be.