农业工程学报
農業工程學報
농업공정학보
2015年
11期
173-178
,共6页
魏霞%李勋贵%Huang Chihua
魏霞%李勛貴%Huang Chihua
위하%리훈귀%Huang Chihua
土壤改良剂%产流%产沙%水土流失%模拟降雨%玉米茎秆汁液
土壤改良劑%產流%產沙%水土流失%模擬降雨%玉米莖稈汁液
토양개량제%산류%산사%수토류실%모의강우%옥미경간즙액
soil conditioner%runoff%sediment%soil and water loss%simulated rainfall%corn stalk juice
该文通过室内人工模拟降雨试验,研究了地表施加玉米茎秆汁液对降雨产流产沙强度的影响,旨在探索玉米茎秆汁液是否可以作为土壤改良剂来减少产流产沙强度。试验设计了2种玉米茎秆汁液的施加量(400和800 g)、4种施加浓度(10%、25%、50%和75%)和4种降雨强度(50、25、75、100 mm/h)。结果表明,各施加浓度和施加量的玉米茎秆汁液都能够减少降雨产流产沙强度,且相同条件下的产沙强度减小程度大于产流强度减小程度。当玉米茎秆汁液的施加量为400 g时,随着施加浓度从10%增加至25%、50%和75%,减流百分比分别为31.243%、31.685%、34.595%和39.475%,减沙百分比分别为23.167%、41.993%、37.918%和64.606%;当玉米茎秆汁液的施加量为800 g时,随着施加浓度从10%增加至25%、50%、75%,减流百分比分别为37.583%、56.433%、63.170%和76.360%,减沙百分比分别为48.214%、77.219%、88.572%和95.539%。当施加量和降雨强度相同时,产流产沙强度与施加浓度之间呈显著的指数函数递减关系,产沙强度随降雨强度的变化呈显著的幂函数递增关系。当施加量为400 g时,各施加浓度下的产流强度与降雨强度之间呈显著的线性函数递增关系,当施加量为800 g时,各施加浓度下的产流强度随降雨强度呈显著的指数函数递增关系。研究为水力侵蚀的防治提供了新思路,为水蚀荒漠化的防治提供了新方法。
該文通過室內人工模擬降雨試驗,研究瞭地錶施加玉米莖稈汁液對降雨產流產沙彊度的影響,旨在探索玉米莖稈汁液是否可以作為土壤改良劑來減少產流產沙彊度。試驗設計瞭2種玉米莖稈汁液的施加量(400和800 g)、4種施加濃度(10%、25%、50%和75%)和4種降雨彊度(50、25、75、100 mm/h)。結果錶明,各施加濃度和施加量的玉米莖稈汁液都能夠減少降雨產流產沙彊度,且相同條件下的產沙彊度減小程度大于產流彊度減小程度。噹玉米莖稈汁液的施加量為400 g時,隨著施加濃度從10%增加至25%、50%和75%,減流百分比分彆為31.243%、31.685%、34.595%和39.475%,減沙百分比分彆為23.167%、41.993%、37.918%和64.606%;噹玉米莖稈汁液的施加量為800 g時,隨著施加濃度從10%增加至25%、50%、75%,減流百分比分彆為37.583%、56.433%、63.170%和76.360%,減沙百分比分彆為48.214%、77.219%、88.572%和95.539%。噹施加量和降雨彊度相同時,產流產沙彊度與施加濃度之間呈顯著的指數函數遞減關繫,產沙彊度隨降雨彊度的變化呈顯著的冪函數遞增關繫。噹施加量為400 g時,各施加濃度下的產流彊度與降雨彊度之間呈顯著的線性函數遞增關繫,噹施加量為800 g時,各施加濃度下的產流彊度隨降雨彊度呈顯著的指數函數遞增關繫。研究為水力侵蝕的防治提供瞭新思路,為水蝕荒漠化的防治提供瞭新方法。
해문통과실내인공모의강우시험,연구료지표시가옥미경간즙액대강우산유산사강도적영향,지재탐색옥미경간즙액시부가이작위토양개량제래감소산유산사강도。시험설계료2충옥미경간즙액적시가량(400화800 g)、4충시가농도(10%、25%、50%화75%)화4충강우강도(50、25、75、100 mm/h)。결과표명,각시가농도화시가량적옥미경간즙액도능구감소강우산유산사강도,차상동조건하적산사강도감소정도대우산류강도감소정도。당옥미경간즙액적시가량위400 g시,수착시가농도종10%증가지25%、50%화75%,감류백분비분별위31.243%、31.685%、34.595%화39.475%,감사백분비분별위23.167%、41.993%、37.918%화64.606%;당옥미경간즙액적시가량위800 g시,수착시가농도종10%증가지25%、50%、75%,감류백분비분별위37.583%、56.433%、63.170%화76.360%,감사백분비분별위48.214%、77.219%、88.572%화95.539%。당시가량화강우강도상동시,산유산사강도여시가농도지간정현저적지수함수체감관계,산사강도수강우강도적변화정현저적멱함수체증관계。당시가량위400 g시,각시가농도하적산류강도여강우강도지간정현저적선성함수체증관계,당시가량위800 g시,각시가농도하적산류강도수강우강도정현저적지수함수체증관계。연구위수력침식적방치제공료신사로,위수식황막화적방치제공료신방법。
Although polyacrylamide and other manufactured soil amendments have been effective in runoff and sediment reduction, there is a need to seek natural products that may provide the same soil conservation benefits. In the process of developing green biomass utilization, such as fiber extraction, the plant juice becomes a natural byproduct because only water is used in the extraction. In this research, corn stalk juice was tested for its effects on runoff generation intensity and sediment yield intensity. The experimental design involved four simulated rainfall intensities (25, 50, 75, and 100 mm/h), four diluted corn stalk juice concentrations (10%, 25%, 50%, and 75%), and two diluted corn stalk juice amounts (400 and 800 g) on four 0.5-m-long, 0.2-m-wide, and 0.1-m-deep soil boxes set at 5% slope. Experiments were conducted at the USDA-ARS National Soil Erosion Research Lab. Surface soil (0-10 cm) of a Crosby-Miami complex alfisol with 20% clay, 66% silt and 14% sand was from the Purdue Animal Science Research and Education Center in West Lafayette, Indiana. The test soil was air-dried, crushed and then passed through an 8-mm sieve. The corn stalk juice used in this study was extracted from field corn plants grown at Purdue Agronomy Farm at West Lafayette, Indiana. A 100-min continuous rainstorm was applied. The storm consisted of four intensity sequences: 50 mm/h for 60 min, 25 mm/hfor 20 min, 75 mm/h for 10 min and 100 mm/h for 10 min. Runoff samples were collected in 1-liter HDPE bottles every 5 min during the two lower intensity rains and every 3 min during the two higher intensity rains. Time to fill the runoff bottle was recorded. After each run, the sample bottles were weighed immediately to obtain the runoff rate. Approximately 5 mL of saturated alum solution was added to the sample bottles to flocculate the suspended sediment. After settling overnight, the excess water was poured off the bottles. The bottles were placed in the oven set at 105°C for at least 24 h or until the sediments were dried. Dry weights were then taken to calculate the sediment delivery rate and concentration. The results showed that all kinds of diluted corn stalk juice applications and concentrations reduced runoff generation intensity and sediment yield intensity. Sediment reduction benefit was greater than the corresponding runoff reduction benefit under the same diluted corn stalk juice application and concentration. When diluted corn stalk juice application was 400 g, runoff reduction ratio was 31.243%, 31.685%, 34.595%, 39.475% and sediment reduction ratio was 23.167%, 41.993%, 37.918%, 64.606% with diluted corn stalk juice concentration increasing from 10% to 25%, 50% and 75%, respectively. When diluted corn stalk juice application was 800 g, runoff reduction ratio was 37.583%, 56.433%, 63.170%, 76.360% and sediment reduction ratio was 48.214%, 77.219%, 88.572%, 95.539% with diluted corn stalk juice concentration increasing from 10% to 25%, 50% and 75%, respectively. The relationships of runoff generation intensity and diluted corn stalk juice concentration, sediment yield intensity and diluted corn stalk juice concentration were both established as decreasing exponential function when diluted corn stalk juice application and rainfall intensity were both same. The relationship between sediment yield intensity and rainfall intensity was established as increasing power function when diluted corn stalk juice application and concentration were both same. However, the relationship between runoff generation intensity and rainfall intensity was relatively complex. When diluted corn stalk juice application amount was 400 g, the relationship between runoff generation intensity and rainfall intensity was established as a significant increasing linear function. When diluted corn stalk juice application amount was 800 g, the relationship between runoff generation intensity and rainfall intensity was established as a significant increasing exponential function. This research can provide a new idea for prevention and control of soil erosion by water, and provide a new method for the prevention and control of water erosion desertification.