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首页> 外文期刊>Animal Production Science >Measurement of soil matric potential under 'Williams' Bon Cretien' pear comparing regulated deficit with normal irrigation
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Measurement of soil matric potential under 'Williams' Bon Cretien' pear comparing regulated deficit with normal irrigation

机译:在“ Williams” Bon Cretien”梨下测量土壤基质势,将调节亏缺与正常灌溉进行比较

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Soil matric potential (SMP) was measured under close planted 'William Bon Cretian' pear (Pyrus communis L.) after a period of withholding irrigation and during a period of regulated deficit irrigation (RDI). Trees were trickle irrigated with 20% replacement of pan evaporation over the planting square (Eps) after an initial period without irrigation, and compared with trees constantly irrigated at 80% Eps. Midway between 2 pairs of trees in each treatment (henceforth the 20% and 80% trees), gypsum blocks were installed in a grid pattern at depths of 10, 25, and 40 cm in the tree line and at 30 and 60 cm on the west and east sides of the tree line, to measure soil matric potential (SMP). The blocks were measured prior to, and 12 h, after irrigation. Consistent with previous results under RDI, shoot growth decreased and yields increased on the 20% relative to the 80% trees. Measured SMPs thus represent suitable levels for RDI. After withholding irrigation, SMPs at the 10 and 25 cm depths ranged between -1.25 and -2.61 MPa in the central position, but were less negative away from the tree line (-0.4 to -2.08) and at the 40 cm depth (-0.35 to -0.91). When averaged over all measurement dates during RDI, pre- and post-irrigation SMPs were more negative at all sites under the 20% compared with the 80% treatments. The pattern of wetting under the 20% treatment was restricted to the central tree line, with some skewing towards the east. Within this soil volume SMP fluctuated between irrigations, and prior to irrigation ranged between -0.3 and -0.7 MPa. As it was likely that only a small fraction of the available subsoil moisture was utilised, available water under the 20% treatment probably was confined to this small volume of soil.
机译:在禁水灌溉期和调节性缺水灌溉期(RDI)之后,在密植的“ William Bon Cretian”梨(Pyrus communis L.)下测量土壤基质势(SMP)。在不进行灌溉的初始阶段之后,对树木进行点滴灌溉,并在种植面积(Eps)上替换20%的锅蒸发量,然后与以80%Eps持续灌溉的树木进行比较。每次处理中两对树木之间的中间位置(此后为20%和80%的树木),将石膏块以网格模式安装在树线的深度为10、25和40 cm处,并在树线的深度为30和60 cm处。在树线的西侧和东侧,以测量土壤基质势(SMP)。在灌溉之前和之后12小时测量块。与以前在RDI下的结果一致,相对于80%的树木,20%的树梢生长减少且产量增加。因此,测得的SMP代表RDI的合适水平。停止灌溉后,中央位置在10和25厘米深度处的SMP范围在-1.25至-2.61 MPa之间,但远离树线(-0.4至-2.08)和40厘米深度(-0.35)处的负值较小至-0.91)。如果将RDI期间所有测量日期的平均值计算出来,则在20%以下的所有地点,灌溉前和灌溉后SMP的阴性率均高于80%处理。在20%处理下的润湿方式仅限于中心树线,有些向东倾斜。在此土壤体积内,SMP在两次灌溉之间波动,并且在灌溉之前介于-0.3和-0.7 MPa之间。由于可能仅利用了少量的可用底土水分,因此经过20%处理的可用水可能仅限于这小部分土壤。

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    《Animal Production Science 》 |1992年第4期| p.487-492| 共6页
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