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Soil Porosity as Affected by Land Management Practices in Sandy Loam and Loamy Sand Soils

机译:土壤陶油层受砂土壤土和壤土土壤中的土地管理实践影响

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摘要

Land management practices significantly affect soil porosity and related characteristics including soil moisture characteristics, soil consistency and water holding capacity. Hence, a field study was conducted with 3 land management practices in mainplots including conventional tillage (CT), no-tillage with residue (NTR) and deep tillage (DT) under 2 textured soils i.e. sandy loam and loamy sand with 3 replications. Soil porosity (%) was found to be significantly higher under DT (0.494 and 0.416) followed by CT (0.478 and 0.399) and least in NTR (0.458 and 0.383) in sandy loam and loamy sand soils, respectively. However, the effect of tillage and residue management practices on soil consistency limits i.e. liquid limit and plastic limits were neither significant nor uniform. The highest liquid limit was found in NTR (45.9) in sandy loam while, the same was highest in DT (39.7) in loamy sand soil. The liquid limits were found to be 36.7 and 44.8 in CT in loamy sand and sandy loam soils, respectively. The plastic limit followed the similar trend with maximumvalue was observed in NTR (19.7 and 22.8) followed by CT (18.8 and 22.2) and least in DT (18.3 and 21.7) in loamy sand and sandy loam soils, respectively. The soil organic carbon content (g kg1) was found to be highest under NTR (4.2 and 4.7) followed byCT (3.8 and 4.1) and least in DT (3.6 and 3.9) in loamy sand and sandy loam soils, respectively. Maximum water holding capacity (%) was observed in NTR (48.2 and 41.3) followed by DT (45.4 and 38.7) and minimum in CT (43.5 and 34.5) in sandy loam and loamy sand soils, respectively. At field capacity (0.3 bar suction) the maximum soil moisture content was observed in NTR (24.3 and 18.1), followed by DT (23.8 and 17.6) and least in CT (22.7 and 17.3) in sandy loam and loamy sand soils, respectively. Meanmaximum GMD (mm) was observed in NTR (1.5 and 1.2) followed by CT (1.3 and 1.1) and least under DT (1.2 and 0.9) in sandy loam and loamy sand soils, respectively.
机译:土地管理实践显着影响土壤孔隙率和相关特征,包括土壤湿度特征,土壤稠度和水持能力。因此,在包括常规耕作(CT)的主要耕作(CT),与残留物(NTR)和深层耕作土壤(DT)的阴膜中进行的田间研究进行了田间研究,其中2个织地不妥的土壤中,即桑迪壤土和3次复制的壤土。发现土壤孔隙率(%)在DT(0.494和0.416)下显着高于CT(0.478和0.399),分别在砂土壤土和壤土土壤中的NTR(0.458和0.383)中。然而,耕作和残留管理实践对土壤稠度限制的影响,即液体限制和塑料限制既不明显也不是均匀的。在砂质壤土中的NTR(45.9)中发现了最高的液体限制,而植物砂土的DT(39.7)中也是最高的。发现液体限制是植物砂和砂土土壤中的CT中的36.7和44.8。在NTR(19.7和22.8)中观察到塑料极限随后在NTR(19.7和22.8)中观察到具有最高值的趋势,然后分别为CT(18.8和22.2),分别在植物砂和砂壤土土壤中的CT(18.3和21.7)中。发现土壤有机碳含量(G kg1)在NTR(4.2和4.7)下是最高的,然后分别在植物砂和砂壤土土壤中的CYCT(3.8和4.1),最小的DT(3.6和3.9)。在NTR(48.2和41.3)中观察到最大水持续容量(%),然后分别在砂土和壤土和壤土中的CT(43.5和34.5)中的DT(45.4和38.7)和最低限度。在现场容量(0.3巴吸入),在NTR(24.3和18.1)中观察到最大土壤水分含量,然后分别在砂土和溶解的沙壤中的CT(22.7和17.3)中的DT(23.8和17.3)。在NTR(1.5和1.2)中观察到CT(1.3和1.1),分别在砂土和壤土和壤土砂土中的CT(1.2和0.9)中观察到的平均GMD(mm)。

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