Elma Tarım Alanlarında Yüzey Toprakların Sınırlandırılmış Su Aralığının Belirlenmesi

Pelin Alaboz, S. Demi̇r, Ahmet Ali Işıldar, Levent Başayiğit
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Abstract

The In recent years, it is expected that the plant obtains optimum benefit from irrigation applied to the soil since the increase of drought due to global warming and the decrease of water resources. That is why, The least limiting water range (LLWR) which is known as an index of the soil quality, draws considerable attention and is defined as the soil water content in which root development limited. In this study, LLWR values of surface soils of the orchards which intensive apple production was made in Boğazova plain, Eğirdir district Isparta province were determined. Spatial distribution of LLWR values, and relations of LLWR with some soil properties was investigated. The medium-fine texture group is dominant in the study and the SSA values of these soils varied between 6.59-19.27 %. LLWR values of soils; It showed statistically positive significant relationships with clay, organic matter and CaCO 3 , and negative with bulk density (P<0.05; P<0.01). The SSA distribution map created using the inverse distance weighting (IDW) spatial distribution method, the root mean square error (RMSE) was determined as 0.98 %. Soils, where LLWR is determined between 15-20 % range, are in the South of the study area and in the southwest of Eğirdir lake. LLWR is determined between 10-15 % range, were generally determined in the North where there are fine textured soils. It was determined that 80 % of these apple orchards, LLWR values were determinde at lower levels than optimum available water capacity as a result of aeration and/or compaction problems. As a result of the study, it was determined that the moisture content of the air filled pore volume is 10 % and the field capacity moisture contents are affected by the problems of aeration and compaction so that the LLWR changed significantly.
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近年来,由于全球气候变暖导致干旱加剧,水资源减少,预计植物将从土壤灌溉中获得最佳效益。因此,作为土壤质量指标的最小限水范围(LLWR)备受关注,它被定义为根系发育受到限制的土壤含水量。本研究测定了伊斯帕塔省Eğirdir区Boğazova平原苹果集约化生产果园表层土壤LLWR值。研究了土壤水分含量的空间分布及其与土壤性质的关系。中细质组土壤的SSA值在6.59 ~ 19.27%之间。土壤LLWR值;与粘土、有机质、caco3呈显著正相关,与容重呈显著负相关(P<0.05;P < 0.01)。采用逆距离加权(IDW)空间分布法建立SSA分布图,确定均方根误差(RMSE)为0.98%。研究区南部和Eğirdir湖西南部的土壤LLWR在15- 20%之间。LLWR在10- 15%的范围内确定,通常在北方有细质地土壤的地方确定。结果表明,由于通风和/或压实问题,80%的苹果园的LLWR值低于最佳有效水量。研究结果表明,充气孔隙体积的含水率为10%,而现场容量含水率受曝气和压实问题的影响,使LLWR发生显著变化。
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