四川大学化学工程学院,四川,成都,610065
纸质出版:2015
移动端阅览
张璐琪, 赵展恒, 王玉娇, 等. 不同沙化土地改良材料对沙化土壤热量传递的影响[J]. 水土保持通报, 2015,35(2):163-166.
ZHANG Luqi, ZHAO Zhanheng, WANG Yujiao, et al. Effects of Different Improvement Materials on Heat Transmission of Desertification Soil[J]. Bulletin of Soiland Water Conservation, 2015, 35(2): 163-166.
张璐琪, 赵展恒, 王玉娇, 等. 不同沙化土地改良材料对沙化土壤热量传递的影响[J]. 水土保持通报, 2015,35(2):163-166. DOI: 10.13961/j.cnki.stbctb.2015.02.032.
ZHANG Luqi, ZHAO Zhanheng, WANG Yujiao, et al. Effects of Different Improvement Materials on Heat Transmission of Desertification Soil[J]. Bulletin of Soiland Water Conservation, 2015, 35(2): 163-166. DOI: 10.13961/j.cnki.stbctb.2015.02.032.
[目的] 研究不同土地改良材料对沙化土壤热量传递关系的影响
以便有效保墒和防治沙漠化。[方法] 分别将4种沙化土地改良材料(无机性沙化土地改良材料、综合性沙化土地改良材料、石膏性沙化土地改良材料、高碳性沙化土地改良材料)按一定比例(5%
7%
9%
11%
12%)与沙化土壤进行混合配制
通过模拟稳态辐射作为土壤沙化过程的热推动力
测定不同土层深度
不同成分的沙化土壤温度。[结果] 不同材料的添加导致土壤导热率发生改变;在-4~-8 cm土层
4种材料以不同比例添加至沙土中后
对导热率的影响为:石膏性沙化土地改良材料 >无机性沙化土地改良材料 >高碳性沙化土地改良材料 >综合性沙化土地改良材料。综合性沙化土地改良材料在该土层范围内最适宜的添加比例为9%。[结论] 综合性沙化土地改良材料和高碳性沙化土地改良材料对沙化土壤的改良效果较佳。
[Objective] The objective is researching different land improvement material's impactions on the heat transmission of desertification soil in order to maintain soil water and control land deserification.[Methods] Using four different improvement materials(inorganic soil improvement material
integrated soil improvement material
gypseous soil improvement material
high-carbon soil improvement material) mixed with desertification soil in different proportions(5%
7%
9%
11%
12%
respectively). Steady state radiation was presumed as the heat impetus of soil degradation process
temperatures in different soil depths and compositions were measured.[Results] Addition of different materials led to the change of soil thermal conductivity. In the depths of -4~-8 cm
the effects on the thermal conductivity of four materials' addition in different proportion to the soil were:gypseous soil improvement material>inorganic soil improvement material>high-carbon soil improvement material>integrated soil improvement material. The best proportion of adding the integrated soil improvement material to the soil in -4~-8 cm depth was 9%.[Conclusion] Integrated soil improvement material and high-carbon soil improvement material are better modified materials for improving desertification soil.
张顺谦, 郭海燕, 罗勇. 气候变化和载畜量对若尔盖草地沙化的驱动力评价[J]. 中国草地学报, 2007, 29(5):64-71.
高志球, 姜冬梅. 土壤热传导方程解析解和那曲地区土壤热扩散率研究[J]. 气象学报, 2002, 60(3):352-360.
Wierenga P J, Nielsen D R, Hagan R M. Thermal properties of a soil based upon field and laboratory measurements[J]. Soil Science Society of America Journal, 1969, 33(3):354-360.
李毅, 邵明安, 王文焰, 等. 质地对土壤热性质的影响研究[J]. 农业工程学报, 2003, 19(4):62-65.
Chen Yongping, Shi Mingheng, Li Xiaochuan. Experimental investigation on heat, moisture and salt transfer in soil[J]. International Communications in Heat and Mass Transfer, 2006, 33(9):1122-1129.
Bird R B, Stewart W E, Lightfoot E N. Transport phenomena[M]. John Wiley & Sons, 2007.
秦耀东.土壤物理学[M].北京:高等敎育出版社,2003.
吴竞仑,李永丰,张志勇,等.土层深度对稻田杂草种子出苗及生长的影响[J].江苏农业学报,2003,19(3):170-173.
0
浏览量
1450
下载量
0
CSCD
关联资源
相关文章
相关作者
相关机构
京公网安备11010802024621