Results 31 to 40 of about 86 (70)
Water, Heat and Solute processes in Seasonally frozen Soils : Experimental and Modeling Study
Soil freezing and thawing is of importance in transport of water, heat and solute, which has coupled effects. Solute type and solute content in frozen soil could influence the osmotic potential of frozen soil and decrease freezing point, resulting in ...
Wu, Mousong
core
Soil freezing/thawing is of importance in the transport of water, heat and solute, with coupled effects. Due to complexity in soil freezing/thawing, uncertainty could be influential in both experimentation and simulation work in frozen soils.
Jansson, Per-Erik, +2 more
core
[Research progress on analytical methods for the determination of hexachlorobutadiene]. [PDF]
Wang Y, Zhang H, Shi J, Jiang G.
europepmc +1 more source
[Annual review of capillary electrophoresis technology in 2020]. [PDF]
Wei B, Ma Y, Tian W, Zhao X, Qu F.
europepmc +1 more source
[Recent advance of new sample preparation materials in the analysis and detection of environmental pollutants]. [PDF]
Feng J +8 more
europepmc +1 more source
为探索石河子灌区冻融季节积雪与地表联合覆盖条件下土壤水盐运移的变化规律,2015—-2016年通过田间小区试验,进行了秸秆、地膜、活性炭3种地表覆盖和裸地对照在整个季节性冻融期土壤水盐时空动态变化规律研究。结果表明:地表覆盖比裸地具有更好的保墒、降盐效果。冻结土壤完全融通后,秸秆、活性炭覆盖出现含水量增幅的最大土层范围分别是0—30,0—40 cm,反映出这2种覆盖经历冻融过程后更有利于土壤水分的保持和融雪水的高效利用;活性炭、秸秆、地膜覆盖和裸地在0—30 cm土层含盐量相比初始值的增幅分别为18 ...
唐文政 +3 more
doaj
[Application of nanocellulose in flexible sensors]. [PDF]
Sun P, Du Y, Yuan X, Hou X, Zhao J.
europepmc +1 more source
[目的] 为研究生物结皮覆盖和冻融作用对土壤结构的影响。[方法] 以黄土高原北部风沙土为研究对象,采用室内模拟冻融的方法,利用田口方法分析不同冻融次数、冻融前土壤初始含水量和生物结皮(藻结皮)盖度对土壤结构特征的影响。[结果] (1)通过正交试验获取的土壤结构指数(IGSS)为75.57~96.57,信噪比(S/N)为37.55~39.70 dB,通过田口方法确定的最佳因子组合为15次冻融循环、15%初始含水量、80%藻结皮覆盖度,其预测结果为IGSS=98.09,S/N=39.89 dB。(2 ...
钟志强 +4 more
doaj
东北黑土区是我国重要的商品粮生产基地,强烈水土流失导致的黑土厚度下降及土壤质量退化,直接威胁国家粮食安全。系统分析黑土区土壤侵蚀研究成果,对阻控黑土退化、维持土地生产力、保障国家粮食安全具有重要意义,论述了黑土区土壤侵蚀环境与侵蚀环境效应、土壤侵蚀过程与机理、土壤侵蚀时空变化和未来研究展望。多营力复合、缓坡长坡是黑土区独特的侵蚀环境,黑土厚度下降与坡耕地土壤质量退化是该区最典型的侵蚀环境效应。细沟间、细沟、浅沟、切沟及冻融侵蚀发育的动力机制与主控因素差异明显 ...
张光辉, 杨扬, 刘瑛娜, 王志强
doaj
目的青藏高原草甸土对气候变化引起的季节性冻融频次改变尤为敏感,亟须揭示草甸土微生物活性对不同冻融循环次数的响应规律。方法选取青藏高原地区季节性冻融作用频繁的高寒草甸土为研究对象,通过非冻融与1、3、5、7、9次冻融循环模拟,对比分析典型土壤可溶性碳氮、微生物碳氮及气体碳氮的响应特征。结果1)与未冻融土壤相比,9次冻融循环后土壤微生物生物量碳显著降低23.64%,可溶性有机碳质量分数显著提升7.37%,CO2和N2O累积释放量分别增加71.09%和321.40%。2) 随着冻融循环次数增加,可溶性有机碳 ...
黄伟, 杨小艺, 李浩乐, 胡亚鲜
doaj

