陕西师范大学学报:自然科学版
陝西師範大學學報:自然科學版
협서사범대학학보:자연과학판
Journal of Shaanxi Normal University: Nat Sci Ed
2012年
3期
87-91
,共5页
马延东%赵景波%古丽扎堤·哈布肯%邢闪
馬延東%趙景波%古麗扎隄·哈佈肯%邢閃
마연동%조경파%고려찰제·합포긍%형섬
海晏县%沙柳林%土壤干层%土壤水库
海晏縣%沙柳林%土壤榦層%土壤水庫
해안현%사류림%토양간층%토양수고
Haiyan county%Salix plantation%soil dry layer%soil reservoir
采用烘干称重法对海晏县城和西海镇附近沙柳林地土壤水分进行研究.结果表明:位于河漫滩上的海晏城附近的沙柳林土壤含水量高,平均含水量为25.1%,土壤水分能够满足沙柳林的正常生长;位于一级阶地上的西海镇沙柳林土壤上部1m范围内含水量较高,平均含水量为19.3%,1m以下含水量很低,有土壤干层发育.这表明,在该区自然降水条件下,除地形低洼、地下水很浅的河漫滩地区之外,土壤水分不能满足人工林正常生长需要.该区沙柳林土壤水分收入小于支出,具有负平衡的特点.该区土壤上部1.0m深度范围内以粉砂为主,孔隙度较高,土质优良,但1.0m以下以粗砂和细砾石为主,土质较差.
採用烘榦稱重法對海晏縣城和西海鎮附近沙柳林地土壤水分進行研究.結果錶明:位于河漫灘上的海晏城附近的沙柳林土壤含水量高,平均含水量為25.1%,土壤水分能夠滿足沙柳林的正常生長;位于一級階地上的西海鎮沙柳林土壤上部1m範圍內含水量較高,平均含水量為19.3%,1m以下含水量很低,有土壤榦層髮育.這錶明,在該區自然降水條件下,除地形低窪、地下水很淺的河漫灘地區之外,土壤水分不能滿足人工林正常生長需要.該區沙柳林土壤水分收入小于支齣,具有負平衡的特點.該區土壤上部1.0m深度範圍內以粉砂為主,孔隙度較高,土質優良,但1.0m以下以粗砂和細礫石為主,土質較差.
채용홍간칭중법대해안현성화서해진부근사류임지토양수분진행연구.결과표명:위우하만탄상적해안성부근적사류림토양함수량고,평균함수량위25.1%,토양수분능구만족사류림적정상생장;위우일급계지상적서해진사류림토양상부1m범위내함수량교고,평균함수량위19.3%,1m이하함수량흔저,유토양간층발육.저표명,재해구자연강수조건하,제지형저와、지하수흔천적하만탄지구지외,토양수분불능만족인공림정상생장수요.해구사류림토양수분수입소우지출,구유부평형적특점.해구토양상부1.0m심도범위내이분사위주,공극도교고,토질우량,단1.0m이하이조사화세력석위주,토질교차.
The oven drying weighing method was used to study the soil water at Salix plantation near Xihai town and Haiyan county. Results showed that the soil moisture content was high on the floodplain near the city of Salix plantation, with an average moisture content of 25.1%, so the soil moisture was able to meet the normal growth of Salix plantation. The soil moisture at 1.0 m depth in the upper part of the soil which located at the first terrace near the city of Salix plantation was much higher, with average moisture content of 19.3%. And the soil moisture below 1 m was very low, which was due to the development of soil dry layer. This suggests that soil moisture couldn't meet the needs of plantation growth under natural conditions of precipitation in the area, apart from low-lying terrain and shallow groundwater in floodplain regions. In this area, the income of soil water was less than its expenditure for Salix plantation, which was a negative balance. The soil at 1. 0 m depth was dominated by silt sand with high porosity and excellent quality, but by poor coarse sand and fine gravel below 1.0 m.