Soil organic matter in biogenic, intermediate and physicogenic aggregates under agroecological management

نویسندگان

چکیده

ABSTRACT Agroecological management can favor the improvement of soil attributes, especially organic matter (SOM) and aggregation. The objective study was to quantify carbon contents humic oxidizable fractions SOM aggregates from different origins agroecological systems. Five experimental areas located in Integrated Production System were evaluated: AFS – Agroforestry System; C-SUN Coffee full sun; C-SHA Shaded coffee; AL-FLE Cultivation alleys Flemingia macrophylla with green beans; NT No-tillage. separated, identified, classified as their origin or formation pathways into biogenic, intermediate, physicogenic. fulvic acid (C-FAF), (C-HAF) humin (C-HUMF); (F1 F2, labile; F3 F4, recalcitrant) determined. greatest variations values observed AFS, In relation C-HUMF, highest this fraction quantified biogenic intermediate C-SUN, showed variability between systems, mainly for F1, F2 under C-SHA. system a higher proportion more humified recalcitrant when compared system. practices maids systems C-SHA, promoted improvements quality.

برای دانلود باید عضویت طلایی داشته باشید

برای دانلود متن کامل این مقاله و بیش از 32 میلیون مقاله دیگر ابتدا ثبت نام کنید

اگر عضو سایت هستید لطفا وارد حساب کاربری خود شوید

منابع مشابه

Soil Aggregates and Associated Organic Matter under Conventional Tillage, No-Tillage, and Forest Succession after Three Decades

Impacts of land use on soil organic C (SOC) are of interest relative to SOC sequestration and soil sustainability. The role of aggregate stability in SOC storage under contrasting land uses has been of particular interest relative to conventional tillage (CT) and no-till (NT) agriculture. This study compares soil structure and SOC fractions at the 30-yr-old Horseshoe Bend Agroecosystem Experime...

متن کامل

Soil organic matter and management of plant-parasitic nematodes.

Organic matter and its replenishment has become a major component of soil health management programs. Many of the soil's physical, chemical, and biological properties are a function of organic matter content and quality. Adding organic matter to soil influences diverse and important biological activities. The diversity and number of free-living and plant-parasitic nematodes are altered by rotat...

متن کامل

Soil pathogen-aphid interactions under differences in soil organic matter and mineral fertilizer

There is increasing evidence showing that microbes can influence plant-insect interactions. In addition, various studies have shown that aboveground pathogens can alter the interactions between plants and insects. However, little is known about the role of soil-borne pathogens in plant-insect interactions. It is also not known how environmental conditions, that steer the performance of soil-bor...

متن کامل

Effects of Straw Incorporation on Soil Organic Matter and Soil Water-Stable Aggregates Content in Semiarid Regions of Northwest China

The soil degradation caused by conventional tillage in rain-fed areas of northwest China is known to reduce the water-use efficiency and crop yield because of reduced soil porosity and the decreased availability of soil water and nutrients. Thus, we investigated the effects of straw incorporation on soil aggregates with different straw incorporation rates in semiarid areas of southern Ningxia f...

متن کامل

Ding Et Al.: Tillage Management Affecting Soil Organic Matter

ganic C (SOC). Soils of the southeastern United States of America, particularly sandy Coastal Plain soils, have Soil organic matter (SOM) is of primary importance for maintaining inherently low SOC contents (typically below 1%, Hunt soil productivity, and agricultural management practices may signifiet al., 1982). Consequently, small changes in the SOM cantly influence SOM chemical properties. ...

متن کامل

ذخیره در منابع من


  با ذخیره ی این منبع در منابع من، دسترسی به آن را برای استفاده های بعدی آسان تر کنید

ژورنال

عنوان ژورنال: Revista Caatinga

سال: 2023

ISSN: ['0100-316X', '1983-2125']

DOI: https://doi.org/10.1590/1983-21252023v36n118rc