Effect of Tillage Systems on Distribution of Aggregates and Organic Carbon in a Long-Term No-Tillage Paddy Field

2011 ◽  
Vol 183-185 ◽  
pp. 1185-1189
Author(s):  
Qi Wen Tang ◽  
Chang Sheng Jiang ◽  
Qing Ju Hao ◽  
Yan Wu
Keyword(s):  
Organic Carbon ◽  
Soil Layer ◽  
Bottom Layer ◽  
Conventional Tillage ◽  
Organic Carbon Content ◽  
Diameter Class ◽  
Tillage Systems ◽  
No Till ◽  
Long Term Experiment

The effect of different tillage systems on the size distribution of aggregates and organic carbon distribution and storage in different size aggregates in a Hydragric Anthrosol were studied in a long-term experiment in Chongqing, China. The experiment included five tillage treatments, which are conventional tillage with rice only system (DP), conventional tillage with rotation of rice and rape system (SH), no-till and ridge culture with rotation of rice and rape system (LM), no-till and plain culture with rotation of rice and rape system (XM) and tillage and ridge culture with rotation of rice and rape system (LF), respectively. The results showed that the aggregates 0.25-0.05 mm in diameter accounted for the largest proportion in each soil layer under all treatments. The organic carbon mainly exist in aggregates in the 0.25-2 mm and 0.05-0.25 mm diameter in the plough layer, which mainly exist in the 0.25-2 mm in diameter in the bottom layer. Distribution of organic carbon in aggregates in the 0.05-0.25 mm diameter class was highest, followed by the aggregates in the 0.25-2mm diameter class. The organic carbon in aggregates under different tillage systems was in a decreasing order of LM (21.05 g·kg-1)> DP (14.13 g·kg-1)> XM (13.29 g·kg-1)> LF (12.54 g·kg-1) > SH (11.41 g·kg-1). The total organic carbon content showed a significant correlation with the amount of aggregates with diameter >0.005 mm. The results showed that the accumulation of soil organic carbon was mainly affected by aggregates in the >0.005mm diameter class.

Tillage Effects on Soil Active Organic Carbon in a Purple Paddy Soil

2011 ◽  
Vol 183-185 ◽  
pp. 2163-2167
Author(s):  
Yan Wu ◽  
Qing Ju Hao ◽  
Chang Sheng Jiang
Keyword(s):  
Organic Carbon ◽  
Soil Depth ◽  
Soil Layer ◽  
Conventional Tillage ◽  
Good Effect ◽  
Tillage Systems ◽  
No Till ◽  
Active Organic Carbon ◽  
Long Term Experiment

The effect of different tillage systems on the soil organic carbon (SOC), active organic carbon (AOC) and remaining organic carbon (ROC) were studied in a long-term experiment in Chongqing, China. The experiment included five tillage treatments, which are conventional tillage with rice only system (DP), conventional tillage with rotation of rice and rape system (SH), no-till and ridge culture with rotation of rice and rape system (LM), no-till and plain culture with rotation of rice and rape system (XM) and tillage and ridge culture with rotation of rice and rape system (LF), respectively. The results showed that the content of SOC declined as the soil depth increased, and presented obvious surface enrichment phenomenon under the no-tillage systems. The order of SOC, AOC, ROC and ROC/SOC in the 0–60 cm soil layer under different tillage systems was LM (22.74 g kg-1) > DP (14.57 g kg-1) > XM (13.73 g kg-1) > LF (13.10 g kg-1) > SH (11.92 g kg-1), DP (3.67 g kg-1) > LF (3.49 g kg-1) > LM (3.28 g kg-1) > XM (3.17 g kg-1) > SH (2.69 g kg-1), LM (18.09 g kg-1) > DP (10.34 g kg-1) > XM (10.12 g kg-1) > LF (9.20 g kg-1) > SH (8.80 g kg-1) and LM (85%) > SH (78%) > XM 77%) > LF (75%) > DP (74%). Compared with other systems, LM significantly increased SOC, ROC and ROC/SOC, which indicated long-term LM system performed good effect for carbon sequestration.

Effect of Tillage Systems on Soil Organic Carbon and Soil Quality in a Purple Paddy Soil

2011 ◽  
Vol 183-185 ◽  
pp. 1190-1194
Author(s):  
Jun Ke Zhang ◽  
Qing Ju Hao ◽  
Chang Sheng Jiang ◽  
Yan Wu
Keyword(s):  
Organic Carbon ◽  
Soil Quality ◽  
Paddy Soil ◽  
Conventional Tillage ◽  
Water Infiltration ◽  
Purple Soil ◽  
Tillage Systems ◽  
Field Station ◽  
No Till ◽  
The Impact

The impact of conservation tillage practices on carbon sequestration has been of great interest in recent years. This experiment analyzed the organic carbon status of soils sampled at depth increments from 0 to 60 cm after 20 years in a purple paddy soil. The tillage experiment was established in the Key Field Station for Monitoring of Eco-Environment of Purple Soil of the Ministry of Agriculture of China, located in the farm of Southwest University (30°26′N, 106°26′E), Chongqing. In this paper, five tillage treatments including conventional tillage with rice only system (DP), conventional tillage with rotation of rice and rape system (SL), no-till and ridge culture with rotation of rice and rape system (LM), no-till and plain culture with rotation of rice and rape system (XM) and tillage and ridge culture with rotation of rice and rape system (LF) were selected as research objectives to measure SOC storage and stratification ratio of SOC (CSR). The SOC storage under different tillage systems was calculated based on an equivalent soil mass. The CSR can be used as an indicator of soil quality because surface organic matter is essential to erosion control, water infiltration, and the conservation of nutrients. Results showed that in soil under no-till SOC was concentrated near the surface, while in tilled soil SOC decreased equably with the increase of soil depth. The difference of SOC contents between the five tillage systems was the largest in the top soil and the lowest in the bottom soil. The order of SOC storage was LM (158.52 Mg C•ha-1) >DP (106.74 Mg C•ha-1) >XM (100.11 Mg C•ha-1) >LF (93.11 Mg C•ha-1) >SL (88.59 Mg C•ha-1), LM treatment was significantly higher than the other treatments. The CSR of 0-10/50-60 cm was 2.65, 2.70 and 2.14 under LM, XM and LF treatments, while 1.54 and 1.92 under DP and SL treatments. We considered CSR>2 indicate an improvement in soil quality produced by changing from tillage to no-tillage, as well as changing from plane to ridge. Overall, long-term LM treatment is a valid strategy for increasing SOC storage and improving soil quality in a purple paddy soil in Southwest China.

scholarly journals Impact of direct seeding mulch-based cropping systems on soil nematodes in a long-term experiment in Madagascar

2009 ◽  
Vol 44 (8) ◽  
pp. 949-953 ◽  
Author(s):  
Cécile Villenave ◽  
Bodovololona Rabary ◽  
Jean-Luc Chotte ◽  
Eric Blanchart ◽  
Djibril Djigal
Keyword(s):  
Cropping Systems ◽  
Soil Layer ◽  
Conventional Tillage ◽  
Direct Seeding ◽  
Living Mulch ◽  
Long Term Experiment ◽  
Tillage System ◽  
Kikuyu Grass ◽  
Structure Indices

The objective of this work was to assess the effects of conventional tillage and of different direct seeding mulch-based cropping systems (DMC) on soil nematofauna characteristics. The long-term field experiment was carried out in the highlands of Madagascar on an andic Dystrustept soil. Soil samples were taken once a year during three successive years (14 to 16 years after installation of the treatments) from a 0-5-cm soil layer of a conventional tillage system and of three kinds of DMC: direct seeding on mulch from rotation soybean-maize residues; direct seeding of maize-maize rotation on living mulch of silverleaf (Desmodium uncinatum); direct seeding of bean (Phaseolus vulgaris)-soybean rotation on living mulch of kikuyu grass (Pennisetum clandestinum). The samples were compared with samples from natural fallows. The soil nematofauna, characterized by the abundance of different trophic groups and indices (MI, maturity index; EI and SI, enrichment and structure indices), allowed the discrimination of the different cropping systems. The different DMC treatments had a more complex soil food web than the tillage treatment: SI and MI were significantly greater in DMC systems. Moreover, DMC with dead mulch had a lower density of free-living nematodes than DMC with living mulch, which suggested a lower microbial activity.

scholarly journals Distribution and vertical stratification of carbon and nitrogen in soil under different managements in the pampean region of Argentina

2011 ◽  
Vol 35 (6) ◽  
pp. 1985-1994 ◽  
Author(s):  
Carina Rosa Álvarez ◽  
Alejandro Oscar Costantini ◽  
Alfredo Bono ◽  
Miguel Ángel Taboada ◽  
Flavio Hernán Gutiérrez Boem ◽  
...  
Keyword(s):  
Soil Layer ◽  
Conventional Tillage ◽  
No Tillage ◽  
Tillage Systems ◽  
Total N ◽  
Organic C ◽  
C Storage ◽  
C Pools ◽  
No Till ◽  
Total Organic C

One of the expected benefits of no-tillage systems is a higher rate of soil C sequestration. However, higher C retention in soil is not always apparent when no-tillage is applied, due e.g., to substantial differences in soil type and initial C content. The main purpose of this study was to evaluate the potential of no-tillage management to increase the stock of total organic C in soils of the Pampas region in Argentina. Forty crop fields under no-tillage and conventional tillage systems and seven undisturbed soils were sampled. Total organic C, total N, their fractions and stratification ratios and the C storage capacity of the soils under different managements were assessed in samples to a depth of 30 cm, in three layers (0-5, 5-15 and 15-30 cm). The differences between the C pools of the undisturbed and cultivated soils were significant (p < 0.05) and most pronounced in the top (0-5 cm) soil layer, with more active C near the soil surface (undisturbed > no-tillage > conventional tillage). Based on the stratification ratio of the labile C pool (0-5/5-15 cm), the untilled were separated from conventionally tilled areas. Much of the variation in potentially mineralizable C was explained by this active C fraction (R² = 0.61) and by total organic C (R² = 0.67). No-till soils did not accumulate more organic C than conventionally tilled soils in the 0-30 cm layer, but there was substantial stratification of total and active C pools at no till sites. If the C stratification ratio is really an indicator of soil quality, then the C storage potential of no-tillage would be greater than in conventional tillage, at least in the surface layers. Particulate organic C and potentially mineralizable C may be useful to evaluate variations in topsoil organic matter.

Effects of Conservation Tillage on Organic Carbon and Carbon Management Index in Paddy Soil

2011 ◽  
Vol 71-78 ◽  
pp. 2759-2762
Author(s):  
Juan Peng ◽  
En Ci ◽  
Zhuo Wang Fu ◽  
Ming Gao ◽  
De Ti Xie
Keyword(s):  
Organic Carbon ◽  
Soil Quality ◽  
Paddy Soil ◽  
Conservation Tillage ◽  
Conventional Tillage ◽  
Tillage Systems ◽  
Carbon Management ◽  
Labile Organic Carbon ◽  
Carbon Management Index

Effects of different tillage systems on organic carbon and carbon management index (CMI) in paddy soil of long-term experiment site (since 1990) were studied. The experiment included three tillage treatments: conventional tillage with rotation of rice and winter fallow (CT-r) system, no-tillage and ridge culture with rotation of rice and rape (RT-rr) system, and conventional tillage with rotation of rice and rape (CT-rr) system. Soil labile organic carbon measured by oxidation of KMnO4 respond rapidly to carbon supply changes, and it is considered as an important indicator of soil quality. Compared with CT-r system, long-term RT-rr system significantly increased total organic carbon and labile organic carbon in surface soil (0-10 cm and10-20 cm). The proportion of labile organic carbon to total organic carbon under RT-rr system was higher than other tillage systems. The carbon management index (CMI) is derived from the total soil organic carbon pool and carbon lability and is useful to evaluate the capacity of management systems to promote soil quality. The CMI increased in each layer under RT-rr system, while it decreased under CT-rr system. This indicated that conservation tillage improved the capacity of the management system into promoting soil quality in Sichuan Basin of China.

scholarly journals Soil physical properties and soil organic carbon content in northeast Brazil: long-term tillage systems effects

2020 ◽  
Vol 77 (4) ◽  
Author(s):  
Fernanda Cristina Caparelli Oliveira ◽  
Gabriel William Dias Ferreira ◽  
João Lucas Santos Souza ◽  
Matheus Emannuel Oliveira Vieira ◽  
Alceu Pedrotti
Keyword(s):  
Organic Carbon ◽  
Soil Organic Carbon ◽  
Physical Properties ◽  
Carbon Content ◽  
Soil Physical Properties ◽  
Organic Carbon Content ◽  
Northeast Brazil ◽  
Tillage Systems ◽  
Soil Organic Carbon Content

scholarly journals Impacts of land-use and management systems on organic carbon and water-physical properties of a Latossolo Amarelo (Oxisol)

2017 ◽  
Vol 38 (1) ◽  
pp. 109 ◽  
Author(s):  
Rodrigo Fonseca da Silva ◽  
Glenio Guimarães Santos ◽  
Júlio César Azevedo Nóbrega ◽  
Geraldo César de Oliveira ◽  
Bruno De Oliveira Dias ◽  
...  
Keyword(s):  
Land Use ◽  
Organic Carbon ◽  
Physical Properties ◽  
Carbon Content ◽  
Weather Conditions ◽  
Conventional Tillage ◽  
Management Systems ◽  
Organic Carbon Content ◽  
Eucalyptus Plantation ◽  
No Till

The Cerrado biome has outstanding territorial relevance in the state of Piauí, in which weather conditions, relief and favorable soil has made this region one reference in food production. This study focused to evaluate the effects of different land uses, management systems and their respective terms on organic carbon content and physical properties of a Latossolo Amarelo (Oxisol) in the Southwestern Piauí state. The study was performed in the city of Uruçuí, situated in the southwestern Piauí state. We assessed nine farming areas with different backgrounds regarding land-use, management system and run time. The treatments consisted of areas under no-till for 3 and 6 years (NT3 and NT6), under pasture for 2 and 5 years (PA2 and PA6), under eucalyptus plantation for six and twelve years (EU6 and EU12), under conventional tillage for two and 8 years (CT2 and CT8) and under native Cerrado (NC), which represented a reference condition. Conversion of the native Cerrado into no-till and grazing areas increased soil organic carbon content over time.

scholarly journals Composição Total Elementar do Solo de um Experimento de Longa Duração Usando Espectroscopia Total de Fluorescência de Raios-X (Total elemental composition of a soil in a long term experiment using X-Ray fluorescence spectroscopy)

2016 ◽  
Vol 9 (3) ◽  
pp. 778
Author(s):  
Viviane Capoane ◽  
Ivan Renato Cardoso Krolow ◽  
Danilo Rheinheimer dos Santos ◽  
Lutécia Beatriz Canalli
Keyword(s):  
Fluorescence Spectroscopy ◽  
Cover Crops ◽  
Conventional Tillage ◽  
Natural Fertility ◽  
No Tillage ◽  
Tillage Systems ◽  
X Ray ◽  
Term Experiment ◽  
Long Term Experiment

Neste trabalho, determinaram-se os teores totais das substâncias químicas presentes em um Latossolo Vermelho aluminoférrico utilizando a técnica de espectroscopia total de fluorescência de raios-X. A pesquisa teve como objetivo criar uma base de dados geoquímica para os solos da região sudoeste do Paraná; comparar os resultados com valores de referência nacional e internacional; avaliar o efeito dos sistemas plantio direto versus convencional de cultivo e; de plantas de cobertura de inverno, na geoquímica do solo de um experimento de longa duração. As coletas de solo se deram em três locais distintos, em três camadas (0-10, 10-20 e 20-40 cm). A técnica utilizada forneceu de maneira rápida e limpa a impressão digital química do solo e os mesmos servem de background para o sudoeste do Paraná. Os teores de elementos químicos preconizados por organizações nacionais e internacionais não estão alinhados com os teores observados em áreas não antropizadas do estado do Paraná. Os resultados obtidos também mostraram que 29 anos após a implantação do experimento, a fertilidade natural foi alterada e que, a substituição da vegetação nativa por sistemas cultivados levou a exportação de algumas substâncias químicas do solo como SO3, MnO, Co e, ao acúmulo de outras como CaO, K2O e MgO. No sistema plantio direto (0-10 cm) concentraram-se os maiores teores de substâncias de origem antropogênica. O sistema convencional de cultivo apresentou diferenciação significativa nos teores entre as plantas de cobertura e não significativa entre as camadas de solo.   A B S T R A C T In this work, the total chemical element levels in a Rhodic Hapludox were determined using total  X-ray fluorescence spectroscopy. The research aimed to create a geochemical database of soils in the southwestern region of Paraná; compare the values obtained with national and international reference values; evaluate the effect of no-tillage versus conventional tillage systems and; coverage plants on the soil geochemistry in a long term experiment. Soil collections were made in three different locations, each in three layers (0-10, 10-20 and 20-40 cm). The technique gave a quick, clean chemical digital impression of the soil which also can be used as a background for the southwestern Paraná. The levels of chemicals recommended by national and international organizations are not aligned with the levels observed in non-disturbed areas of Paraná State. The results also showed that twenty nine years after the beginning of the experiment, the natural fertility changed and that, with the substitution of native vegetation for cultivation systems, levels of some components such as SO3, MnO and Co decreased and those of others such as CaO, K2O and MgO increased. In soils for which no-tillage systems (0-10 cm) is the largest concentrations of anthropogenic substances. The conventional tillage systems gave levels very different from those found in soils under coverage plants and not significantly different between the soil layers. Keywords: soil management, cover crops, no tillage, conventional tillage, geochemistry.   

scholarly journals Effects of 24 Years of Conservation Tillage Systems on Soil Organic Carbon and Soil Productivity

2013 ◽  
Vol 2013 ◽  
pp. 1-10 ◽  
Author(s):  
Kenneth R. Olson ◽  
Stephen A. Ebelhar ◽  
James M. Lang
Keyword(s):  
Organic Carbon ◽  
Soil Organic Carbon ◽  
Conservation Tillage ◽  
Soil Productivity ◽  
Tillage Systems ◽  
No Till ◽  
Plot Area ◽  
Chisel Plow ◽  
Moldboard Plow

The 24-year study was conducted in southern Illinois (USA) on land similar to that being removed from Conservation Reserve Program (CRP) to evaluate the effects of conservation tillage systems on: (1) amount and rates of soil organic carbon (SOC) storage and retention, (2) the long-term corn and soybean yields, and (3) maintenance and restoration of soil productivity of previously eroded soils. The no-till (NT) plots did store and retain 7.8 Mg C ha−1more and chisel plow (CP) −1.6 Mg C ha−1less SOC in the soil than moldboard plow (MP) during the 24 years. However, no SOC sequestration occurred in the sloping and eroding NT, CP, and MP plots since the SOC level of the plot area was greater at the start of the experiment than at the end. The NT plots actually lost a total of −1.2 Mg C ha−1, the CP lost −9.9 Mg C ha−1, and the MP lost −8.2 Mg C ha−1during the 24-year study. The long-term productivity of NT compared favorably with that of MP and CP systems.

scholarly journals Tracking Changes on Soil Structure and Organic Carbon Sequestration after 30 Years of Different Tillage and Management Practices

Agronomy ◽  
2021 ◽  
Vol 11 (2) ◽  
pp. 291
Author(s):  
Ramón Bienes ◽  
Maria Jose Marques ◽  
Blanca Sastre ◽  
Andrés García-Díaz ◽  
Iris Esparza ◽  
...  
Keyword(s):  
Triticum Aestivum ◽  
Organic Carbon ◽  
Management Practices ◽  
Management Strategies ◽  
Triticum Aestivum L ◽  
Field Trials ◽  
Conventional Tillage ◽  
Soil Parameters ◽  
Wilting Point

Long-term field trials are essential for monitoring the effects of sustainable land management strategies for adaptation and mitigation to climate change. The influence of more than thirty years of different management is analyzed on extensive crops under three tillage systems, conventional tillage (CT), minimum tillage (MT), and no-tillage (NT), and with two crop rotations, monoculture winter-wheat (Triticum aestivum L.) and wheat-vetch (Triticum aestivum L.-Vicia sativa L.), widely present in the center of Spain. The soil under NT experienced the largest change in organic carbon (SOC) sequestration, macroaggregate stability, and bulk density. In the MT and NT treatments, SOC content was still increasing after 32 years, being 26.5 and 32.2 Mg ha−1, respectively, compared to 20.8 Mg ha−1 in CT. The SOC stratification (ratio of SOC at the topsoil/SOC at the layer underneath), an indicator of soil conservation, increased with decreasing tillage intensity (2.32, 1.36, and 1.01 for NT, MT, and CT respectively). Tillage intensity affected the majority of soil parameters, except the water stable aggregates, infiltration, and porosity. The NT treatment increased available water, but only in monocropping. More water was retained at the permanent wilting point in NT treatments, which can be a disadvantage in dry periods of these edaphoclimatic conditions.

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