Figures & data
Figure 1 The experimental design showing different treatments including no-till (NT) and chisel-till (CT) under drainage (TD) and non-drainage (ND) systems at the Waterman Farm of Ohio State University, Columbus, OH.
![Figure 1 The experimental design showing different treatments including no-till (NT) and chisel-till (CT) under drainage (TD) and non-drainage (ND) systems at the Waterman Farm of Ohio State University, Columbus, OH.](/cms/asset/3fea4da7-e4ca-4879-b420-1b18ec82a78e/tssp_a_878643_f0001_oc.jpg)
Table 1 Soil organic carbon (SOC) and total nitrogen (TN) concentrations influenced by long-term no-till and chisel-till under drainage and non-drainage systems for the 0–10 and 10–20 cm depths, and analysis of variance
Table 2 Soil organic carbon (SOC) and total nitrogen (TN) concentrations influenced by long-term no-till and chisel-till under drainage and non-drainage systems for the 20–40 and 40–60 cm depths, and analysis of variance
Figure 2 Soil organic carbon stock (SOC, Mg ha−1) as influenced by tillage (A; NT, no-tillage, and CT, chisel-tillage) and drainage (B; D, drainage, and ND, no-drainage) systems for the 0–10, 10–20, 20–40 and 40–60 cm depths.
![Figure 2 Soil organic carbon stock (SOC, Mg ha−1) as influenced by tillage (A; NT, no-tillage, and CT, chisel-tillage) and drainage (B; D, drainage, and ND, no-drainage) systems for the 0–10, 10–20, 20–40 and 40–60 cm depths.](/cms/asset/a9d9de42-d134-4172-85b0-ce8f1a325021/tssp_a_878643_f0002_b.gif)
Figure 3 Soil carbon stored in heavy (HF-C) and light (LF-C) fractions of carbon under long-term tile drainage (TD) and non-drainage (ND) systems for the 0–10, 10–20, 20–40 and 40–60 cm depths.
![Figure 3 Soil carbon stored in heavy (HF-C) and light (LF-C) fractions of carbon under long-term tile drainage (TD) and non-drainage (ND) systems for the 0–10, 10–20, 20–40 and 40–60 cm depths.](/cms/asset/d76ba342-36a2-480c-8da9-1391ebb4f968/tssp_a_878643_f0003_b.gif)
Figure 4 Soil nitrogen stored in heavy (HF-N) and light (LF-N) fractions of nitrogen under long-term tile drainage (TD) and non-drainage (ND) systems for the 0–10, 10–20, 20–40 and 40–60 cm depths.
![Figure 4 Soil nitrogen stored in heavy (HF-N) and light (LF-N) fractions of nitrogen under long-term tile drainage (TD) and non-drainage (ND) systems for the 0–10, 10–20, 20–40 and 40–60 cm depths.](/cms/asset/ee4e43d4-85a2-4a6e-ae85-ae0f287f5e88/tssp_a_878643_f0004_b.gif)
Table 3 Microbial biomass carbon (MBC) for the 0–10 and 10–20 cm depths under no-till and chisel-till of drainage and non-drainage systems, and analysis of variance
Table 4 Water stable aggregates (WSA) and mean weight diameter (MWD) for no-till and chisel-till under drainage and non-drainage systems for the 0–10 cm depth, and analysis of variance
Table 5 Corn (Zea mays L.) yield for 2006 through 2012 as influenced by tillage and drainage systems