2020
DOI: 10.3390/su12125019
|View full text |Cite
|
Sign up to set email alerts
|

Determining Soil Hydraulic Properties Using Infiltrometer Techniques: An Assessment of Temporal Variability in a Long-Term Experiment under Minimum- and No-Tillage Soil Management

Abstract: Conservation agriculture is increasingly accepted by farmers, but the modeling studies on agro-environmental processes that characterize these agricultural systems require accurate information on the temporal variability of the soil’s main physical and hydraulic properties. Therefore, specific investigations carried out in long-term experiments can increase our knowledge on the pros and cons of different measurement techniques. In this work, the simplified falling head (SFH) technique and the Beerkan Estimatio… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
3
2

Citation Types

1
9
0

Year Published

2021
2021
2022
2022

Publication Types

Select...
7
1

Relationship

4
4

Authors

Journals

citations
Cited by 13 publications
(10 citation statements)
references
References 50 publications
1
9
0
Order By: Relevance
“…In this regard, it is worth noting that while the expected positive relationship between compost rate and TOC or AC returns an increasing sequence of treatments (i.e., T1 < T2 < T3 < T4), a different positioning around the regression line is obtained when the effects on conductive features are considered (Figures 7 and 8, respectively), probably due to a negligible effect of the fertilizer dose (T2). The rationale used to interpret our findings, successfully applied in other investigations both in natural [33,40] and agricultural [41] environments, however, was not applicable when the full dataset (initial + ending soil sampling) or when only initial soil condition (initial soil sampling) was considered (Table 4). This result seems obvious enough and may be attributed to the lack of soil structure after box setup.…”
Section: Discussionmentioning
confidence: 99%
“…In this regard, it is worth noting that while the expected positive relationship between compost rate and TOC or AC returns an increasing sequence of treatments (i.e., T1 < T2 < T3 < T4), a different positioning around the regression line is obtained when the effects on conductive features are considered (Figures 7 and 8, respectively), probably due to a negligible effect of the fertilizer dose (T2). The rationale used to interpret our findings, successfully applied in other investigations both in natural [33,40] and agricultural [41] environments, however, was not applicable when the full dataset (initial + ending soil sampling) or when only initial soil condition (initial soil sampling) was considered (Table 4). This result seems obvious enough and may be attributed to the lack of soil structure after box setup.…”
Section: Discussionmentioning
confidence: 99%
“…Intensive agricultural activity and not sustainable management practices may give rise to soil degradation processes with a consequent decline of crop yield and soil quality [4,7], and an associated reduction in ecosystem functions and services [8,9]. Among land-use and soil management practices, tillage strongly affects soil physical quality since it directly modifies soil aggregation and structural stability [10], soil porosity [11,12] and hydrological properties [13] and thus the soil ability to store and transmit water and air [14,15]. In addition, tillage management plays a key role in soil organic matter turnover, microbial abundance and diversity, carbon storage and thus CO 2 emissions [16,17].…”
Section: Introductionmentioning
confidence: 99%
“…Usually, high BD and PR values are linked to lower soil porosity, so lower Ks values were expected relative to those observed. However, contrasting results on the effects of reduced tillage on Ks also appear in the literature (Blanco-Canqui and Ruis, 2020;Castellini et al, 2020;Strudley et al, 2008). Indeed, some studies (e.g., Lipiec et al, 2006;Pagliai et al, 2004) have found how the presence of biopores from root decomposition and earthworm activity might alleviate soil compaction by promoting preferential flow through macropores, while other studies (e.g., Kahlon et al, 2013;Vogeler et al, 2009) have suggested that the loss of macroporosity under no-tillage may not sustain water infiltration.…”
Section: Discussionmentioning
confidence: 99%