Comparing the short- and long-term impacts of subsurface drainage installation on soil physical and biological properties

被引:0
作者
Frankl, A. L. [1 ]
Sherbine, K. T. [1 ,2 ]
Strock, J. S. [3 ]
Fernandez, F. G. [1 ]
Cates, A. M. [1 ]
Pease, L. A. [4 ]
机构
[1] Univ Minnesota, Dept Soil Water & Climate, St Paul, MN 55108 USA
[2] USDA ARS, Davis, CA USA
[3] Univ Minnesota, Southwest Res & Outreach Ctr, Dept Soil Water & Climate, Lamberton, MN USA
[4] Univ Minnesota, Dept Soil Water & Climate, Northwest Res & Outreach Ctr, Crookston, MN USA
关键词
potentially mineralizable carbon; saturated hydraulic conductivity; soil biological activity; soil physical properties; SATURATED HYDRAULIC CONDUCTIVITY; PREFERENTIAL FLOW PATHS; ORGANIC-CARBON LOSSES; AGGREGATE STABILITY; BULK-DENSITY; DIFFERENT TILLAGE; CLAY SOILS; HOT-SPOTS; WATER; CROP;
D O I
10.2489/jSWC.2023.00147
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
Subsurface drainage is a common practice used to support agricultural production and increase yields in poorly drained soils. Following decades of subsurface drainage instal-lation, agricultural fields often have increased water discharge and nutrient losses. However, few studies have evaluated the changes in soil properties or soil health metrics at different ages of subsurface drainage. In this study, we attempt to quantify changes to soil properties over time. To achieve this, we sampled six fields in northwest Minnesota representing two timescales: three fields were drained more than 15 years prior to sampling (i.e., subsurface drainage installed prior to 2006), and three fields were drained within 5 years of sampling (i.e., subsurface drainage installed after 2016). We evaluated three soil physical properties: saturated hydraulic conductivity (Kfs), bulk density, and aggregate stability, as well as three soil health metrics at 0 to 15 and 15 to 30 cm: water-extractable organic carbon (WEOC) and nitro-gen (WEON), and potentially mineralizable carbon (PMC). The fields with older drainage systems had greater Kfs, WEON (all depths), WEOC (15 to 30 cm), and PMC (15 to 30 cm). There were no differences in bulk density, aggregate stability, WEOC (0 to 15 cm), and PMC (0 to 15 cm). We suspect that the increased Kfs is likely the result of further development of preferential flow pathways in fields with older drainage systems. These preferential flow paths could also be areas with increased microbial diversity and activity, indicated by the higher biological indicators in the fields with older drainage systems. Our findings suggest that nutri-ent losses, soil physical properties, and soil health metrics evolve over time. These metrics should be tracked as a standard practice in drainage research to improve our understanding of how subsurface drainage installation changes long-term soil properties. This knowledge will improve the information provided to growers and help them more effectively manage their soil's health and reduce nutrient losses into waterways.
引用
收藏
页码:457 / 465
页数:9
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