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 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.

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.

scholarly journals Effect of Conservational and Conventional Tillage Systems on Functional Soil Archaea Diversity in Wheat-Pea Rotation Field

2017 ◽  
Vol 9 (11) ◽  
pp. 34
Author(s):  
E. Essel ◽  
Lingling Li ◽  
Chaochao Deng ◽  
Junhong Xie ◽  
Renzhi Zhang ◽  
...  
Keyword(s):  
16S Rrna ◽  
Soil Depth ◽  
Conventional Tillage ◽  
Rrna Gene ◽  
Tillage Systems ◽  
Linear Discriminant ◽  
Sequencing Platform ◽  
No Till ◽  
Depth Analysis ◽  
Rotation Field

Soil borne archaea in agricultural systems is crucial for cycling of nutrient such as Nitrogen, Carbon and Sulphur. The objective of the study was to assess the effect of different tillage systems on functional archaea diversity in a 15 years cereal-legume rotation field using Illumina sequencing platform for archaea 16S rRNA gene. The treatments in the study included conventional tillage with stubble removed (T), no-till with stubble removed (NT), conventional tillage with stubble incorporated (TS) and no-till with stubble retained (NTS). The results showed that the dominant soil archaea phyla was Crenarchaeota (> 96%), followed by Euryarchaeota with a lower abundance of < 3% and then Parvarchaeota and other bacteria phyla made up < 1% across the treatments and depths. The treatment means were ranked as NT > NTS > TS > T for 16S rRNA number of OTUs, Shannon and Simpson indices calculated for the 0-10cm soil depth. Analysis of factor effect revealed that tillage but not stubble retention or their interaction significantly influenced (P < 0.01 and P < 0.05) 16S rRNA diversity. Non metric Multidimensional Scaling (NMDS) analysis clearly grouped the microbial communities according to depths. Linear Discriminant Analysis Effect Size (LEfSe) identified Crenarchaeota and Thaumarchaeota (to genus level) as significantly enriched clades in 0-10 cm depth of T while Euryarchaeota and Thermoplasmata were significantly enriched in TS. The conservational tillage systems (NT and NTS) promoted even distribution of archaea diversity while conventional tillage systems (T and TS) enriched the archaea communities identified in the study.

Effects of a single cycle of tillage on long-term no-till prairie soils

2009 ◽  
Vol 89 (4) ◽  
pp. 521-530 ◽  
Author(s):  
C D Baan ◽  
M C. J Grevers ◽  
J J Schoenau
Keyword(s):  
Organic Carbon ◽  
Soil Organic Carbon ◽  
Crop Production ◽  
Soil Depth ◽  
P Uptake ◽  
Soil Conditions ◽  
Available Phosphorus ◽  
No Till ◽  
Particulate Soil

A study was conducted to examine the effect of tillage on soil conditions and crop growth at three long-term (> 10 yr) no-till sites, one in each of the Brown, Black, and Gray soil zones of Saskatchewan. The four tillage treatments consisted of one cycle of tillage at three levels of intensity: spring cultivation only, fall + spring cultivation, and fall + spring + disc cultivation, all applied to no-till and also a no-till control. Total and particulate soil organic carbon, soil pH, and soil aggregation were not affected by the tillage operations. Tillage decreased the bulk density in the 5- to 10-cm soil depth, but did not affect soil water content (0-10 cm) or spring soil temperature (0-5 cm). Tillage decreased stratification of available phosphorus to some extent, but there appeared to be no associated effect on crop P uptake. Tillage did not effect crop production in any of the 3 yr following its imposition, except at one site where, in the first year, apparent tillage-induced nutrient immobilization resulted in lower yields. Overall, the imposition of one cycle of tillage on long-term no-till soils appears to have little effect on soil properties or crop growth.Key words: No-till, nutrient stratification, soil organic carbon, tillage

Soil nutrient stratification and uptake by wheat after seven years of conventional and zero tillage in the Northern Grain belt of Canada

2006 ◽  
Vol 86 (5) ◽  
pp. 767-778 ◽  
Author(s):  
N Z Lupwayi ◽  
G W Clayton ◽  
J T O’Donovan ◽  
K N Harker ◽  
T K Turkington ◽  
...  
Keyword(s):  
Nutrient Uptake ◽  
Soil Depth ◽  
Soil Layer ◽  
Conventional Tillage ◽  
Wheat Crop ◽  
Zero Tillage ◽  
Tillage Systems ◽  
Nitrate N ◽  
Ammonium N ◽  
Nutrient Stratification

The distribution of NaHCO3-extractable nitrate-N, ammonium-N, phosphorus (P) and potassium (K) with soil depth (0 to 20 cm in 5-cm increments) at Fort Vermilion (58°23′N 116°02′ W), Alberta, was described in the 7th and 8th years of conventional and zero tillage following placement of red clover (Trifolium pratense) green manure (GM), field pea (Pisum sativum), canola (Brassica rapa) and monoculture wheat (Triticum aestivum) residues. Soil nitrate-N concentrations under zero tillage were greater than those under conventional tillage in the 0–5 cm soil layer, below which the concentrations were similar. Ammonium-N and K concentrations followed a similar pattern. However, soil P concentrations were usually not different between tillage systems in the 0–5 cm soil layer, but the concentrations decreased more under zero tillage than under conventional tillage at lower depths. A notable exception for soil phosphate was under canola residues, where the concentration was greater under zero tillage than under conventional tillage at all depths. Uptake of N, P or K by a subsequent wheat crop was usually greater (though not always significantly) under zero tillage than under conventional tillage, and there were no interactions between tillage and crop residue. Therefore, differences in nutrient stratification between the two tillage systems did not translate into differences in wheat nutrient uptake. Key words: Conservation tillage, crop rotation, nutrient uptake, soil nitrogen, soil phosphorus, soil potassium

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 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.

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