干旱地区农业研究
榦旱地區農業研究
간한지구농업연구
AGRICULTURAL RESEARCH IN THE ARID AREAS
2013年
5期
161-167
,共7页
韩玉国%武亨飞%杨培岭%丁涛%辛显华%孙敏%宋贺%李延云
韓玉國%武亨飛%楊培嶺%丁濤%辛顯華%孫敏%宋賀%李延雲
한옥국%무형비%양배령%정도%신현화%손민%송하%리연운
保水剂%饱和含水率%饱和导水率%扩散率%入渗模拟
保水劑%飽和含水率%飽和導水率%擴散率%入滲模擬
보수제%포화함수솔%포화도수솔%확산솔%입삼모의
Super Absorbent Polymer%saturated water content%saturated hydraulic conductivity%soil water diffusiv-ity%infiltration simulation
保水剂在农业上的应用对于缓解干旱具有重要的意义,但其应用后会发生降解而最终失去保水作用,因此了解其在降解过程中引起的土壤物理性质的动态变化及水分运动的机理,是其能否正确应用的关键,本试验以保水剂在农业应用中的典型用量为基础,研究了保水剂对土壤的物理性质动态影响及一维土壤水分。结果表明,保水剂施入土壤后其性能不断衰减是导致土壤物理性质不断变化的最根本原因;土壤中施用保水剂后土壤的质量饱和含水率明显增加,饱和导水率降低,但随着保水剂性能的逐渐衰减,饱和含水率呈现下降趋势,饱和导水率呈现上升趋势;施入保水剂后土壤的扩散率是一个曲面,并且随着保水剂自身性能的衰减,呈现逐渐扩展的趋势;施用保水剂后土壤入渗的湿润锋前进速度下降,这主要是由于施用保水剂土壤的饱和含水量增加和保水剂膨胀堵塞土壤孔隙造成的;通过对施用保水剂土壤的扩散率和导水率的分时段研究,最终建立施用保水剂土壤的一维水分运动方程抄эθ/эt=э/эz D (θ,T )эθ/эz -эK (θ,T )/эz,试验证明其可行,且精度在允许的范围内。
保水劑在農業上的應用對于緩解榦旱具有重要的意義,但其應用後會髮生降解而最終失去保水作用,因此瞭解其在降解過程中引起的土壤物理性質的動態變化及水分運動的機理,是其能否正確應用的關鍵,本試驗以保水劑在農業應用中的典型用量為基礎,研究瞭保水劑對土壤的物理性質動態影響及一維土壤水分。結果錶明,保水劑施入土壤後其性能不斷衰減是導緻土壤物理性質不斷變化的最根本原因;土壤中施用保水劑後土壤的質量飽和含水率明顯增加,飽和導水率降低,但隨著保水劑性能的逐漸衰減,飽和含水率呈現下降趨勢,飽和導水率呈現上升趨勢;施入保水劑後土壤的擴散率是一箇麯麵,併且隨著保水劑自身性能的衰減,呈現逐漸擴展的趨勢;施用保水劑後土壤入滲的濕潤鋒前進速度下降,這主要是由于施用保水劑土壤的飽和含水量增加和保水劑膨脹堵塞土壤孔隙造成的;通過對施用保水劑土壤的擴散率和導水率的分時段研究,最終建立施用保水劑土壤的一維水分運動方程抄эθ/эt=э/эz D (θ,T )эθ/эz -эK (θ,T )/эz,試驗證明其可行,且精度在允許的範圍內。
보수제재농업상적응용대우완해간한구유중요적의의,단기응용후회발생강해이최종실거보수작용,인차료해기재강해과정중인기적토양물이성질적동태변화급수분운동적궤리,시기능부정학응용적관건,본시험이보수제재농업응용중적전형용량위기출,연구료보수제대토양적물이성질동태영향급일유토양수분。결과표명,보수제시입토양후기성능불단쇠감시도치토양물이성질불단변화적최근본원인;토양중시용보수제후토양적질량포화함수솔명현증가,포화도수솔강저,단수착보수제성능적축점쇠감,포화함수솔정현하강추세,포화도수솔정현상승추세;시입보수제후토양적확산솔시일개곡면,병차수착보수제자신성능적쇠감,정현축점확전적추세;시용보수제후토양입삼적습윤봉전진속도하강,저주요시유우시용보수제토양적포화함수량증가화보수제팽창도새토양공극조성적;통과대시용보수제토양적확산솔화도수솔적분시단연구,최종건립시용보수제토양적일유수분운동방정초эθ/эt=э/эz D (θ,T )эθ/эz -эK (θ,T )/эz,시험증명기가행,차정도재윤허적범위내。
Super Absorbent Polymer (SAP) is of important significance in mitigating agricultural drought .However , its role in water retention ultimately fades away due to its degradation after application .Therefore ,the investigation of the dynamic change of soil physical properties and the mechanism of moisture movement caused by degradation of SAP is the key for its proper application .Based on the typical amount of SAP used in agriculture ,the dynamic impacts of SAP on soil physical properties and one-dimensional soil moisture were analyzed .The results showed that the attenuation of SAP performance after its application into soil was the most fundamental reason for the constant change of soil physical proper-ties .After treated with SAP ,the saturated mass water content of soil was significantly increased ,and the saturated hy-draulic conductivity was reduced .However ,as the SAP performance attenuated ,the saturated moisture content showed a downward trend and the saturated hydraulic conductivity showed an upward trend .After treated with SAP ,the water dif-fusivity of soil exhibited a curved surface and showed a gradually expanding trend with the attenuation of its performance . The forward speed of moist sharp point of infiltration in SAP-treated soil was reduced ,which was mainly because that the saturated moisture content of soil was increased and the soil pores were clogged due to the expansion of SAP after it was applied .By investigating the water diffusivity and hydraulic conductivity of SAP-treated soil at different time periods ,a one-dimensional water movement equation was finally established as эθ/эt=э/эz D (θ,T )эθ/эz -эK (θ,T )/эz .It was proved to be feasible with the accuracy within an allowable range .