干旱地区农业研究
榦旱地區農業研究
간한지구농업연구
AGRICULTURAL RESEARCH IN THE ARID AREAS
2015年
2期
122-129
,共8页
张子卓%张珂萌%牛文全%薛万来
張子卓%張珂萌%牛文全%薛萬來
장자탁%장가맹%우문전%설만래
微润灌溉%埋深%压力水头%番茄生长状况%土壤水分动态
微潤灌溉%埋深%壓力水頭%番茄生長狀況%土壤水分動態
미윤관개%매심%압력수두%번가생장상황%토양수분동태
Moistube-irrigation%burying depth%working pressure%growth characteristics of tomato%soil moisture dynamics
为探明微润灌溉对番茄生长和土壤水分的影响,设置了3种不同埋深和2种不同工作压力,研究了微润带埋设深度和压力对番茄生长、产量及水分利用效率的影响。结果表明:定植后94天,微润带压力水头为180 cm 、埋深为15 cm 时的番茄株高分别比埋深10 cm 和20 cm 的处理增加9.17%和7.55%;此时番茄气孔导度最小,光合速率和水分利用效率最大,分别比埋深为10 cm 和20 cm 的处理增产3.24%和7.45%;不同埋深土壤含水率垂直分布随时间的变化存在差异,15 cm 埋深时的土壤含水率最大。微润带埋深是影响土壤水分时空变化的主要因素;压力对土壤含水量时间变化影响不显著。
為探明微潤灌溉對番茄生長和土壤水分的影響,設置瞭3種不同埋深和2種不同工作壓力,研究瞭微潤帶埋設深度和壓力對番茄生長、產量及水分利用效率的影響。結果錶明:定植後94天,微潤帶壓力水頭為180 cm 、埋深為15 cm 時的番茄株高分彆比埋深10 cm 和20 cm 的處理增加9.17%和7.55%;此時番茄氣孔導度最小,光閤速率和水分利用效率最大,分彆比埋深為10 cm 和20 cm 的處理增產3.24%和7.45%;不同埋深土壤含水率垂直分佈隨時間的變化存在差異,15 cm 埋深時的土壤含水率最大。微潤帶埋深是影響土壤水分時空變化的主要因素;壓力對土壤含水量時間變化影響不顯著。
위탐명미윤관개대번가생장화토양수분적영향,설치료3충불동매심화2충불동공작압력,연구료미윤대매설심도화압력대번가생장、산량급수분이용효솔적영향。결과표명:정식후94천,미윤대압력수두위180 cm 、매심위15 cm 시적번가주고분별비매심10 cm 화20 cm 적처리증가9.17%화7.55%;차시번가기공도도최소,광합속솔화수분이용효솔최대,분별비매심위10 cm 화20 cm 적처리증산3.24%화7.45%;불동매심토양함수솔수직분포수시간적변화존재차이,15 cm 매심시적토양함수솔최대。미윤대매심시영향토양수분시공변화적주요인소;압력대토양함수량시간변화영향불현저。
In order to verify the effects of moistube-irrigation on the growth of tomato and water condition of soil , three different buried depths and two different pressure heads were designed .In addition ,the resulting the effects were further analyzed on the growth and yield of tomato and water use efficiency .The results showed that after 94 days of planting ,the buried depth at 15 cm had the highest plants which were increased by 9 .17% and 7 .55% from the buried depths at 10 cm and 20 cm ,respectively .At this time ,tomatoes had the minimal stomata conductance and highest pho-tosynthetic rate and WUE within all of the four treatments employed in this investigation ,resulting in yield increases of 3 .24% and 7 .45% more at buried depth at 15cm than those at buried depths at 10 cm and 20 cm ,respectively .The temporal variations of soil water content along vertical distribution were different under different buried depths ,with the buried depth at 15 cm the highest .The buried depth of moistube was the main factor influencing the temporal variations of soil water content .However ,the effects of temporal variations of soil water content under different pressures were sec -ondary .