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Land use and management impacts on structure and infiltration characteristics of soils in the North Appalachian region of Ohio

机译:土地使用和管理对俄亥俄州北部阿巴拉契亚地区土壤的结构和渗透特征的影响

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摘要

Effects of land use and management treatments on soil mechanical and hydrological properties were assessed by analysis of balk and core soil samples and water infiltration measurements in the field, using double ring infiltrometers in five plots located at the experimental farm of the North Appalachian Experimental Watersheds (NAEW) near Coshocton, Ohio. The five treatments were no-till without manure (NTWM), no-till with manure (NTM), no-till corn (Zee mays)-soybean (Glycine max) rotation (NTCSR), conventional tillage (CT), and meadow (M). Treatments significantly influenced water infiltration characteristics, soil bulk density (rho(b)), aggregation, and mean weight diameter (MWD). The maximum cumulative infiltration after 3 h (I) of 109.3 +/- 29.0 cm (average of 9 measurements at 3 landscape positions) was measured for the NTM treatment and the lowest of 27.7 +/- 21.0 cm (average of 3 measurements at shoulder slope or S) for the CT treatment. The infiltration rate at 5 min (i(5)), steady state infiltration rate after 3 h (i(c)) and field capacity water content 24 h after the infiltration (FC) were higher in NTM (1.5 cm min(-1), 0.4 cm min(-1), and 0.35 gg(-1), respectively) than other treatments. The least values of i(5), i(c) and FC (0.4 cm min(-1), 0.18 cm min(-1), and 0.22 gg(-1), respectively) were observed for the CT treatment. Saturated hydraulic conductivity (K.) measured on soil cores was the highest for the NTM (0.29 cm min(-1)) for 0 to 10 cm and NTCSR (0.24 cm min(-1)) for 10 to 20 cm depth. The rho(b) (1.52 g cm(-3) for 0 to 10 cm and 1.62 g cm(-3) for 10 to 20 cm depth) was the lowest and water stable aggregates (WSA) were the highest (WSA of 89% and 63%) for both depths for the NTM treatment. The rho(b) was much higher for the CT (1.75 g cm(-3) for 0 to 10 cm depth) and NTWM (1.77 g cm(-3) for 10 to 20 cm depth) than NTM, NTCSR and M treatments for either depth. The landscape positions did not have a significant influence on soil physical and water transmission properties nor on total biomass. The manuring treatment improved soil aggregation and water transmission properties (NTM > NTWM > NTCSR).
机译:在北阿巴拉契亚实验集水区实验农场的5个样地中,使用双环渗透仪在田间进行田间和核心土壤样品分析以及水渗透测量,从而评估了土地利用和管理措施对土壤机械和水文特性的影响( NAEW)在俄亥俄州科肖克顿附近。这五种处理方式分别为免耕免耕(NTWM),免耕加肥(NTM),免耕玉米(Zee mays)-大豆(Glycine max)轮作(NTCSR),常规耕作(CT)和草甸( M)。处理对水的渗透特性,土壤容重(rho(b)),聚集和平均重均粒径(MWD)有显着影响。对于NTM处理,测量3 h(I)后的最大累积浸润为109.3 +/- 29.0 cm(在3个风景位置上进行9次测量的平均值),最低为27.7 +/- 21.0 cm(在肩部进行3次测量的平均值)斜率或S)进行CT治疗。 NTM(1.5 cm min(-1)较高,在5 min(i(5))的入渗率,3 h(i(c))后的稳态入渗率和24 h(FC)入渗后的田间持水量较高。 ),0.4 cm min(-1)和0.35 gg(-1)分别)。在CT治疗中观察到i(5),i(c)和FC的最小值(分别为0.4 cm min(-1),0.18 cm min(-1)和0.22 gg(-1))。 NTM(0.29 cm min(-1))在0到10 cm深度和NTCSR(0.24 cm min(-1))在10到20 cm深度时在土芯上测得的饱和导水率(K.)最高。 rho(b)(0至10 cm的1.52 g cm(-3)和10至20 cm的深度的1.62 g cm(-3))最低,水稳性骨料(WSA)最高(WSA为89 NTM处理的两个深度分别为%和63%)。 CT(0至10 cm深度为1.75 g cm(-3))和NTWM(10至20 cm深度为1.77 g cm(-3))的rho(b)比NTM,NTCSR和M处理高得多对于任何深度。景观位置对土壤的物理和水传输特性以及总生物量均无显着影响。粪肥处理改善了土壤的团聚和水分传输特性(NTM> NTWM> NTCSR)。

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