Water infiltration rate in Yellow Latosol under different soil management systems

Cunha, Jorge Luíz Xavier Lins; Coelho, M.F.B.; Albuquerque, Abel W. de; Silva, Cicero A.; Júnior, Antônio Barbosa da Silva; Carvalho, Islan Diego Espindula de

doi:10.1590/1807-1929/agriambi.v19n11p1021-1027

Cited by 15 publications

(14 citation statements)

References 15 publications

(16 reference statements)

Supporting

Mentioning

Contrasting

Unclassified

Order By: Relevance

“…Soil losses due to erosion, reduction of organic matter, compaction, reduction of porosity, and permeability, are some of the consequences of poor use of the soil resource. This investigation disagreed with the results found by other authors (Cunha et al 2015;Kamimura et al 2009;Pinheiro et al 2009) when they studied the infiltration rates in different soil management systems (conventional, minimal and no-tillage), they concluded that minimal cultivation provided higher values of soil water infiltration rate. This difference can often be associated with different soil classes, contribution of organic matter, soil quality, different climate and the time of use in the areas.…”

Section: Resultscontrasting

confidence: 99%

Water infiltration rate in the soil under different uses and covers in the Poxim River basin, Sergipe, Brazil

Batista¹,

Filho²,

Carvalho³

et al. 2020

Int J Innov Educ Res

View full text Add to dashboard Cite

Watersheds are units of planning and environmental management having a great importance in the management of water resources and their use. To this end, knowledge about the soil's physical and water attributes is of paramount importance in the context of water dynamics in aquifer recharge areas. Water infiltration rate into the soil is considered an important variable in the hydrological cycle, as the increase in this process can lead to a reduction in erosion and consequently greater groundwater recharge. Thus, the present work aimed to evaluate the soil water infiltration rate in the phytophysiognomy of the Poxim River basin in the State of Sergipe, in the agriculture, eucalyptus and forest areas, and to observe the effect of the infiltration water rate in areas of no-till, minimum and conventional cultivation. The soil water infiltration rate was obtained through the use of double cylinder infiltrometer and estimated through the mathematical models of Kostiakov, Kostiakov-Lewis, Horton and Philip. When making comparisons between the models for estimating of soil water infiltration rates, the Horton model showed a better fit compared to the other models used, and the type of soil cover that obtained the highest infiltration rate was the forest. No-till areas provided higher water infiltration rates in the soil, contributing to greater groundwater recharge.

show abstract

Section: Resultscontrasting

confidence: 99%

Water infiltration rate in the soil under different uses and covers in the Poxim River basin, Sergipe, Brazil

Batista¹,

Filho²,

Carvalho³

et al. 2020

Int J Innov Educ Res

View full text Add to dashboard Cite

show abstract

“…Puddling and other tillage practices obliterated pore connectivity, and lower aggregate stability caused clogging of pores during infiltration (Kukal & Aggarwal, 2002). There have been contrasting reports of higher infiltration rates (e.g., Das et al, 2018 (due to better pore connectivity) and Thierfelder & Wall, 2010 (due to residue retention and better aggregation)), lower infiltration rates (e.g., Liu, Zhang, Kravchenko, & Iqbal, 2015 (due to the lower amount of macropores in clay textured soil)) or no change (Cunha et al, 2015;Singh, Phogat, Dahiya, & Batra, 2014) in the infiltration rate through adoption of no-tillage or reduced tillage. A global metanalysis concluded there was higher soil infiltration rate with longer duration of adoption of no-tillage (Mondal, Chakraborty, Bandyopadhyay, & Aggarwal, 2019a,b).…”

Section: Discussionmentioning

confidence: 99%

Short‐term (5 years) impact of conservation agriculture on soil physical properties and organic carbon in a rice–wheat rotation in the Indo‐Gangetic plains of Bihar

Mondal

Poonia

Mishra

et al. 2019

European J Soil Science

View full text Add to dashboard Cite

Short-term (5 years) impact of tillage and residue management practices on physical properties and organic carbon (OC) of a silty clay soil was evaluated in a rice-wheat rotation in the Indo-Gangetic Plains of Bihar. The experiment had three conservation agriculture (CA) practices: one full (direct-seeded rice (DSR)-no-tilled wheat (NTW)-no-tilled mung bean (NTMB); fCA) and two partial (puddled transplanted rice (PTR)-NTW-conventionally tilled mung bean (CTMB); pCA1 and unpuddled transplanted rice (UPTPR)-conventionally tilled potato+maize (CTP + M)-NTMB; pCA2), which were evaluated against full conventional practice (puddled transplanted rice (PTR)-conventionally tilled wheat (CTW); TA). Subsurface compaction reduced and soil aggregation improved under both full and partial CA. Macro-and water-stable aggregates increased to a large extent (26 and 11%, respectively) in full CA and to a lesser extent in partial CA, mostly due to increase in coarse macroaggregate (2-8 mm) contents in the 0-10 and 10-20-cm depth soil layers. Steady-state infiltration rate nearly doubled under full CA, with larger pore volume recorded in 10-20 and 20-30-cm depth soil layers. The CA increased OC associated with all size fractions of aggregates in the surface soil layer (0-10 cm), but a higher amount of C was associated with macroaggregates, indicating relative stabilization of OC in the soil under CA. Change in bulk soil OC was larger in the 0-10-cm depth soil layer in favour of CA, which also had an 11% increase in OC stock in the 0-30-cm depth soil layer. Improvement in soil physical condition did not effectively translate into increased rice or wheat yields, but the system productivity increased largely. Highlights • Conservation agriculture (CA) resulted in 11-12% higher macro-aggregation compared to conventional practice (CT). • Macro-and total pores reduced in the 0-10 cm depth soil layer but increased in the 10-20 cm depth soil layer under CA. • CA resulted in 27-35% higher aggregate-associated OC content and 11% increase in OC stock at 0-30 cm.

show abstract

“…In relation to the mathematical adjustments, it can be observed that the model that best adjusted the BIV was the one of Horton, that in all the managements obtained the result equal to the one obtained in the field. Cunha et al (2015), where the methodologies of Kostiakov, Kostiakov-Lews and Horton were also used.…”

Section: Resultsmentioning

confidence: 99%

“…I -estimated instantaneous infltration rate, mm h-1; residual mass ratio (RMR), adjustment coefficient (AC) and efficiency (EF) as described by CUNHA et al (2015).…”

Section: Modelo De Kostiakovmentioning

confidence: 99%

Stable Infiltration Rate in a Yellow Red Argissol in Corn Crop and Guandu Coverage

Santos¹,

Filho²,

Pedrotti³

et al. 2017

Anais Do IV Inovagri International Meeting - 2017

View full text Add to dashboard Cite

This research was carried out in an area in the rural campus of the Federal University of Sergipe (UFS), which studies the impact of soil management changes on production and physical soil attributes during fifteen years. The area was divided into three portions, treated with no-tillage, minimum tillage and conventional tillage. The aim of this work was to compare the stable infiltration rate in a yellow red Argisol in different managements and in a succession of sweet corn and guandu as soil cover, analyzing the impact of the agricultural use and the suitability of the Horton models (1940), Kostiokov (1932), Kostiokov-Lewis (1945) and Phillip (1957). The stable infiltration rate was determined in each plot using the double concentric ring methodology. The VIBK software was used to determine the estimated values of the stable infiltration rate by the mathematics models. In order to evaluate the performance of the infiltration values obtained in the field in relation to the values calculated by the models, comparative analyzes of the results were performed statistically through the determination coefficient (R 2 ). Statistical indices were also determined, such as residual mass coefficient (RMC), coefficient of adjustment (CA) and efficiency (EF

show abstract

Water infiltration rate in Yellow Latosol under different soil management systems

Cited by 15 publications

References 15 publications

Water infiltration rate in the soil under different uses and covers in the Poxim River basin, Sergipe, Brazil

Water infiltration rate in the soil under different uses and covers in the Poxim River basin, Sergipe, Brazil

Short‐term (5 years) impact of conservation agriculture on soil physical properties and organic carbon in a rice–wheat rotation in the Indo‐Gangetic plains of Bihar

Stable Infiltration Rate in a Yellow Red Argissol in Corn Crop and Guandu Coverage

Contact Info

Product

Resources

About