Long Term Resource Conservation Technologies Sustained Yield, Microbial Activities and Soil Physico-chemical Properties in Rice-green Gram Cropping System

Purpose Microbial communities in rhizospheric soil play a signicant role in sustaining the soil quality and also recognized as key ecological indicators to assess the soil health. Methods We studied the long-term effects of resource conservation technologies on functional microbial diversity and their interactions with soil biochemical properties and enzymatic activities in tropical rice-green gram cropping system. The experiment included conventional practice (CC), brown manuring (BM), green manuring (GM), wet direct drum sowing (WDS), zero tillage (ZT), green manuring-customized leaf colour chart based-N application (GM-CLCC N) and biochar (BC) treatments. Results The result revealed that microbial biomass nitrogen (N), carbon (C) and phosphorus (P) in GM practice increased by 23.3, 37.7 and 35.1%, respectively over CC. The Shannon index and McIntosh index were higher by 86.9% and 29.2% in GM as compared to conventional practice and signicantly correlated with microbial biomass (C & P) and soil microbial populations whereas, Shannon index was positively correlated with the microbial biomass (C, N & P) and soil enzyme activities. Principal component analysis showed a signicant separate cluster among the treatments amended with and without biomass addition. Conclusions Moreover, dominance of carbon utilizing microbes in biomass amended treatments indicated that these could supply good amount of labile carbon sources on real time basis for microbial activity. Which may protect the stable carbon fraction in soil, hence could support higher build-up of carbon in long run and could offer sustainable yield under rice-green gram soil. these demonstrated be showed N however was correlated with less interaction as compared to BC. The rst dimension PC1 could explain the variances of four treatments with GM showing maximum variances followed by CC, WDS and GM-CLCCN. Similarly, the second dimension PC2 could explain the maximum variances of only one treatment ZT. The other two treatments BM and BC had less contribution on overall variances represented by PCA. Contribution (coecient values given in parenthesis) of the parameters were higher in DHA (0.915), A (0.912), F (0.910), MBN (0.905), H (0.903), MBP (0.886). As shown in the PCA ordination biplot, it could be inferred these highly correlated parameters to be chiey associated with GM and GM-CLCC N. The parameters CL (0.849), IN (0.815), XY (0.812), MI (0.808), TOC (0.799), AP (0.783), PC (0.741), PO (0.739), AWCD (0.733), AK (0.726) variances was found to be attributed the ZT treatment. MBC (0.723), AN (0.715), FDA (0.723), BG (0.704), UR (0.703) demonstrated lesser variances and from the ordination biplot could be attributed to GM and GM-CLCCN treatments. The treatments CB (-0.405), AA (-0.606) and SI (-0.648) showed negative correlation with GM and GM-CLCC N treatments, however was positively correlated with CC treatment followed by WDS. In the second dimension PC2, the components NM (0.730) and CM (0.72b) showed the highest contribution which can be attributed to GM and GM-CLCC N treatments. The parameters CA (0.450), EC (0.396) were found to have very low correlation coecient in rst dimension PC1, whose contribution increased in third dimension (0.730). However, only the rst two dimensions were taken for analysis.


Introduction
The relationships of soil microorganisms and ecosystems are highly complex. The soil biota are essential for several ecosystem functions including nutrientcycling, biomass decomposition, soil organic matter (SOM) restoration and maintenance of plant health ( Zhang et al., 2012;Dossou-Yovo et al., 2016;Dash et al., 2017;Kumar et al., 2017). However, microbial population structure and their function in soils were in uenced by several environmental factors (Kibblewhite et al., 2008) and the addition of different soil amendments (Benbi et al., 2016) , which could alter the soil characteristics Shahid et al., 2017). Soil microbes also interact directly with soil environment as well as their extracellular enzyme activities that play a vital role in decomposition process for nutrients (carbon, nitrogen, phosphorous and sulphur) availability (Hartmann et al., 2006). These indicators suit for assessing soil microbial activities which improve the soil fertility resulting crop growth productivity (Acosta-martínez et al., 2011;Min et al., 2016). Different resource conservation technologies (RCTs) are now being popular due to concerns about soil fertility deterioration as a consequences of exhaustive tillage practices (Ladha et al., 2003). Resource conservation practices like zero tillage; biomass retention etc. have minimized soil erosion, enhanced nutrient conservation and fetched low economic input (Lal, 2004). The researchers are also assessing the economic turn outs different nutrient management practices and tillage operations under RCTs to understand the behaviour of soil biochemical properties. However, such nutrient management in resource conservation practices affect soil microbial diversities both structural and functional and thereby in uence the soil biochemical properties (Cookson et al., 2007).
Applications of chemicals and fertilizers affect the soil biota and their functions (Anderson, 2003;Weber et al., 2008;Su et al., 2015;Kumar et al., 2017;Shahid et al., 2017). The direct effects include shift in soil pH and heavy metals accumulation which negatively impacted the soil microbiota (Zhang et al., 2012;Turner et al., 2013;Chen et al., 2016). The indirect effects through stimulation of the soil microbiota activity and of crop growth due to higher residues inputs and rhizo-depositions to soil (Su et al., 2015;Tang et al., 2016). Studies conducted under different climatic regimes have shown that the extracellular enzymatic activities respond towards minimum modi cations in the environmental conditions and organic and mineral fertilization management practices, tillage operations and applications of pesticides and herbicides (Tejada et al., 2008;E. Liu et al., 2014;Jacobsen and Hjelmsø, 2014;Wezel et al., 2014). The βglucosidase is an important soil quality indicator used to evaluate the impacts of different cultural practices on physicochemical properties and organic matter stabilization in soil (García-Gil et al., 2000;Badiane et al., 2001). Other enzymes like dehydrogenase, uorescein di-acetate, urease, cellulase etc. are also good indicators of soil fertility (Wanjiru et al., 2015;Tautges et al., 2016).
Long-term resource conservation practices are valuable for residue management and evaluation the residual effects of tillage on soil microbial diversities (both structural and functional) (Lienhard et al., 2013;Pandey et al., 2014). Long-term application of soil amendments (both inorganic and organic) affect the soil microbial communities in different agro-ecosystems (Zhong and Cai, 2007;Baudoin et al., 2009;Wanjiru et al., 2015). Pro ling of different carbon source utilization by groups of soil microbes under different fertilization treatments can be signi cantly generated by using Biolog eco-plates (Kumar et al., 2017).
Some researchers reported that measurement of soil microbial diversity through Biolog alone is not a valid method (Zhou et al., 2008;Tan et al., 2013), however, it gives the indication towards functional microbial diversity.
Rice-green gram system is a widely practiced cropping system in India (Raja et al., 2015;Shahid et al., 2017) however, information on long-term effect of resource conservation practices involving different sources of organic matter and methods of incorporation into the soil in rice-green gram cropping system are lacking. Further, the effect of rice-green gram system on soil fertility due to temporal shifts of functional microbial diversity in rhizospheric soil is also limited. Hence, the objectives of the study were formulated to nd out the effects of resource conservation technologies on (i) soil chemical and biological properties, and changes of functional diversity of soil microbial communities and (ii) to study the relationship among microbial biomass (C, N & P), and soil enzymes in rice-green gram system.

Experimental setup
The study area of the long-term resource conservation technology was situated at ICAR-National Rice Research Institute (NRRI), Cuttack (20º 44' N,85º 94' E) and continuously practiced for ve years. The climate of this area has sub-humid tropical. The annual mean precipitation is around 1500 mm; occurred during the month of June-September and the minimum and maximum mean annual temperatures were 22.5 C and 39.2 C, respectively. The soils of the experimental eld were classi ed as 'Aeric Endoaquept' having a sandy clay loam texture (17% silt, 30% clay and 56% sand). Some of the initial characteristics of the surface soil (0-15 cm) were as follows: pH was 6.6 (using soil: water suspension, 1:2.5); electrical conductivity (EC) 0.49 dS m -1 ; bulk density 1.40 Mg m -3 ; total organic C 6.7 g Kg -1 ; available P 22.8 mg kg -1 ; and available K 265 mg kg -1 ; respectively.
The study was conducted during dry season of 2016-17 in the long-term experiment of resource conservation technologies which has been initiated in 2012.
There were total seven (7) treatments and arranged in a completely randomized block design (CRBD). The treatments were conventional practice (CC), brown manuring (BM), green manuring (GM), wet direct drum sowing (WDS), zero tillage (ZT), green manuring + CLCC-N (GM-CLCC N) and biochar (BC) application, which were replicated thrice (experimental details are given in Table 1). Rice-rice system was followed for initial two years (2012-2014) and then rice-green gram system for three years . In our experiment, rice and green gram; varieties were Pooja and Samrat, respectively. The line × plant spacing was 20 × 15 cm in rice and 30 × 10 cm in green gram. The recommended dose of fertilizer (RDF) for N: P 2 O 5 : K 2 O were at the rate of 80: 40: 40 kg ha −1 for at basal and rest (25%) each at two top dressings to rice. However, the entire N fertilizer was applied in green gram as basal dose. The single superphosphate (SSP) and muriate of potash (KCl) was applied as phosphorus and potassium fertilizer, respectively only as basal dose. Under green and brown manuring treatments, 25% less of nitrogen fertilizer was given in the wet season of rice. At the rate of 25 kg ha -1 , Sesbania aculeata was sown for both the treatments. The 25 days old Sesbania aculeata were knocked down in green manuring treatments by using cono-weeder; however, in brown manuring treatment, Sesbania was killed with the help of 2, 4-D. The real time N-management was done with the help of customized leaf colour chart (CLCC). In biochar treatment at the The soil samples were collected during dry season of 2016-17 after harvesting of the crop (green gram) at four places randomly from each treatment at 0-15 cm depth by using sample probe. The soil collected was mixed thoroughly and homogenize properly to prepare the composite soil for all the treatments separately. One set of fresh soil samples which was used for biochemical as well as microbial analysis were kept at 4 °C in refrigerator, and rest portion of the soil soil was air dried in shade for 7 days and then processed, through 2 mm sieve and stored in seal container for further analysis.
Soil physico-chemical properties Soil pH (soil: water::1: 2.5) and electrical conductivity (EC) were analysed in soil with water suspension and soil saturation extract, respectively by using standard methods. Total organic carbon was estimated by potassium dichromate (K 2 Cr 2 O 7 ) along with sulphuric acid (H 2 SO 4 ) and 85% o-phosphoric acid (H 3 PO 4 ) digestion mixture with a ratio of 3:2 by wet digestion method in a digestion block set for 2h at 120 ºC temperature (Snyder and Trofymow, 1984). Available nitrogen (AN) (Hati et al., 2008), available phosphorus (AP) (Bray R.H and Kurtz L.T, 1945) and available potassium (AK) (Hati et al., 2007) were analysed using standard methods.
Biological properties of soil Soil microbial biomass carbon (MBC) was estimated by using chloroform fumigation-extraction method in which, one set of soil sample was fumigated in vacuum desiccator while other was kept un-fumigated (Witt et al., 2000). Microbial biomass nitrogen (MBN) was analysed following the method of Ross, 1990. Dehydrogenase (DHA) activity was estimated by the formation of 2,3,5-triphenylformazan (TPF) as a result of the reduction of 2, 3, 5triphenyltetrazolium chloride (TTC) (Casida et al., 1964). Fluorescein di-acetate (FDA) hydrolysis and β-glucosidase activities were measured by following the method of Adam andDuncan, 2001 andEivazi andTabatabai, 1988, respectively. Urease activity was estimated by following the method of P. Bhattacharyya et al., 2012. The C and N mineralization were determined by incubating the soil samples for one month. After, incubation the C mineralization (C min ) was estimated followed by alkali traps method (Mohanty et al., 2013). However, for N mineralization (N min ), the mineral N (both NH 4 -N and NO 3 -N) was determined by extraction with 2 M KCl of the incubated soil samples (Abera et al., 2012). Finally, the net N and C mineralization were estimated and the cumulative N min and C min were determined. The aerobic heterotrophic bacterial, fungal and actinomycetes populations were enumerated by adopting the procedure of (Kumar et al., 2017).

Soil microbial community and functional diversity
Soil microbial activity and diversity in the rhizospheric soil was investigated by using Biolog plates (Biolog Inc., CA, USA). Biolog plate consists of 96 wells consisted of one control along with 31 different carbon sources with three replications each. Equivalent to 10 g dry weight of fresh soil sample was taken in a 250 ml conical ask, then 100 ml of distilled water was added and put it in a shaker for 30 minutes at 250 rpm. Then the soil suspension was diluted to 10 -3 and 150 µL of this nal suspension was inoculated in a Biolog plate and incubated at 25 ºC. After incubation of 0, 24, 48, 72, 96 and 120 h, carbon utilization by the microbial community by taking the absorbance of each well at 590 nm. The data were recorded using Microlog 4.01 and to assess total microbial activity the average well color development (AWCD) of the all carbon sources was measured as: Where, C and R refer to the optical density (OD) value of the reaction wells and control well, respectively (Li et al., 2012). The AWCD re ects the overall utilization of different carbon sources by the soil microbial community (Choi and Dobbs, 1999).

Functional diversity analysis by utilizing different carbon sources
The McIntosh (U) and Shannon-Weaver (H) indices were estimated from absorbance of the Biolog eco-plates that express the functional microbial diversity of soil. The Shannon-Weaver index is sensitive to the species richness of the microbial diversity and it is calculated by the formula: "pi refers to the ratio of relative absorbance (C-R) of i th well to the sum of relative OD values of all the wells.
Similarly, McIntosh index is the measurements of species evenness of the microbial community and it was quanti ed by using following formula.
ni, refers to the relative OD for each of the carbon source wells by subtracting the OD value of control well (Guanghua et al., 2008;An et al., 2014).

Relative yield
Relative yield was calculated from mean seasonal rice and rice equivalent (green gram) yields, which was expressed as Mg ha -1 .

Rice equivalent yield (REY):
The equivalent yield was estimated in kharif crop (rice) by using the equation.
Where, MSP= minimum support price.

Statistical analysis
Analysis of variance (ANOVA) of individual character and means were compared with DMRT at signi cant level (p≤0.05) was done by online software version OP STAT. The microbial biomass and activities were analysed by using the coordinate of the points obtained by the principal component analysis (PCA) method in two ways ANOVA. The OD values taken from the Biolog eco-plates of 31 different carbon sources utilization were used to perform the analysis.
Multi-element vectors describing the metabolism of microbial communities were obtained from the PCA analysis. The six major carbon classes were made by using 31 kind of different C sources, then the AWCD values of six major classes of carbon sources were normalized in Microsoft excels and analysed by ANOVA and PCA using the SAS (9.2) software.

Relative yield
Relative yield of the experiment was found in the range of 4.19-4.95 Mg ha -1 and it was signi cantly more under green manuring (GM; 4.95 Mg ha -1 ) and lowest under biochar (BC) treatment (4.19 Mg ha -1 ) ( Fig. 1).

Soil physico-chemical and biological activities
Soil physico-chemical as well as biological properties were in uenced by different resource conservation practices. The pH of the soils in different treatments ranged from 6.6 to 6.8 and was found to be non-signi cant. Electrical conductance (EC) was varied from 0.46 to 0.48 dS m -1 among the treatments. Total organic carbon was ranged from 6.8 to 8.7 g Kg -1 and was signi cantly higher under zero tillage practice compared to others. Highest available N content was also recorded under green manuring (326.1 kg ha 1 ), followed by biochar and brown manuring treatments. Similarly, highest available phosphorous (P) and potassium (K) contents were recorded under green manuring, followed by zero tillage and brown manuring treatments.
Microbial biomass carbon was in the range of 157.1 µg g -1 in control to 252.3 µg g -1 in green manuring treatments, whereas, MBN and MBP in the resultant soils were ranged from 24.5 µg g -1 to 31.9 µg g -1 and 12.8 µg g -1 to 19.7 µg g -1 , respectively. The MBC, MBN and MBP were signi cantly more in green manuring amended plots compared to other treatments, however, signi cantly lower value of these parameters was found in control treatment. The activity of cellulase was varied in the range of 0.31 to 0.98 μg glucose g -1 d -1 . The C min and N min were signi cantly more in plots treated with green manure than other treatments ( Table 2). The content of dehydrogenase activity (DHA), uorescein di-acetate activity (FDA), β-glucosidase activity, urease activity was found signi cantly higher in all resource conservation treatments as compared to control, while the highest activity was observed in green manuring treatment (Table  3). Similarly, cellulase, invertase and xylanase activities of soil were also signi cantly higher under all resource conservation treatments as compared to control, however, the higher activity was observed in zero tillage treatment (Table 3). Among different conservation treatments, the population of aerobic heterotrophic bacteria, fungi and actinomycetes were varied from 6.78 to 6.92 log CFU g -1 , 4.55 to 4.75 log CFU g -1 , 4.47 to 4.72 log CFU g -1 , respectively (Table   3). And the, green manuring treatment recorded the signi cantly (p ≤ 0.05) higher population of these microbes. (ds m -1 ) (g kg -1 ) (kg ha -1 ) (kg ha -1 ) (kg ha -1 ) (µg C g -1 ) (µg N g -1 ) (µg P g -1 ) (µg C g -1 ) (µg N g -1 ) CC  Average well color development showed differences in the metabolic reaction rate of microbial communities among resource conservation treatments. The development of colour based an average utilization of carbon sources using Biolog eco-plates usually showed an S-shaped pattern in relation to time during the 120h incubation-period (Fig. 2). For the duration of incubation, different sources of carbon mineralization by microbes were signi cantly higher in green manuring (GM) than other treatments irrespective of the duration of incubation. The AWCD values in control (CC) were the lowest while under green manuring; the values were found to be highest in all the incubation periods (Fig. 2).
The rate of change in microbial metabolic activities was observed maximum at 48 h of incubation and in the order of GM > BM > ZT > WDS > GM + CLCC-N > CC > BC. After 48 h, the metabolic activities of all the treatments were reduced signi cantly, while, the rate of microbial activities were enhanced in all treatments up to 96 h of incubation and then decreased gradually (Fig. 3).
The AWCD value observed at 72 h of incubation was also higher (26.6%) in green manuring treatment than others. The Shannon index has shown a signi cantly higher values in GM by 86.9% as compared to the control treatment and the lowest was recorded under WDS treatment. The McIntosh index determined from the 72 h incubation period of Biolog ® data was also higher in GM by 29.2% than that of control. The AWCD, Shannon index and McIntosh indices indicated a signi cantly higher microbial activity under GM compared to the RCTs and control (Table 4).  was higher in green manuring (GM) followed by GM-CLCC-N treatment and lowest in control. However, relative stable C compounds like, amines (AM), phenolic compounds (PC) and polymers (PO) utilization were found higher in control treatment followed by WDS, ZT and BC (Fig. 4).
The amines and amino acid utilizing microbes were dominant in all the treatments under resource conservation (Fig. 4). The consumption of carbohydrates and carboxylic acids were found to be highest in CC and BM, respectively, whereas BM showed the highest consumption of amines and GM towards amino acids. However, there was no signi cant difference among all the treatments in the consumption of phenolic compounds and polymers (Fig. 4).

Principal component coupled with biplot analysis
Biplot analysis of seven treatments showed different spatial distribution on the coordinate axis. The corresponding projective points indicate that the BM, GM-CLCC-N treatment plots were in one quadrant and showed signi cantly utilization of amines (AM). Similarly, GM, ZT in another quadrant which gives strong response to amino acids (AA). Biochar detached from all the treatments, occupied a separate quadrant and gives strong response to carboxylic acids (CA).
WDS and CC inhabited in same quadrant, which showed signi cant utilization of carbohydrates (CB), phenolic compounds (PC) and polymers (PO) (Fig. 5 A).
Similarly, biplot analysis of six major groups of speci c kinds of carbon sources, such as carboxylic acid; amino acids; amines; carbohydrates, phenolic compounds and polymers were laid at the 1 st , 2 nd , 3 rd and 4 th quadrant, respectively (Fig. 5 A).
PCA was applied to the dataset consisting of seven treatments (BM, BC, CC, GM, GM-CLCC N, WDS and ZT) in three replications having a total of thirty parameters. As shown in Fig. 5 B. PCA explained a total variance of 65% with PC1 contributing to 51.7% and PC2 contributing to 13.3% respectively. The seven treatments has been found to aggregate into de nite clusters displayed as elliptical circles over the ordination planes, with the larger symbols in centre of each ellipse representing the mean of three replications. In the rst ( WDS and CC inhabited in same quadrant, which showed signi cant utilization of carbohydrates (CB), phenolic compounds (PC) and polymers (PO) (Fig. 5 A).
Similarly, biplot analysis of six major groups of speci c kinds of carbon sources, such as carboxylic acid; amino acids; amines; carbohydrates, phenolic compounds and polymers were laid at the 1 st , 2 nd , 3 rd and 4 th quadrant, respectively (Fig. 5 A).
PCA was applied to the dataset consisting of seven treatments (BM, BC, CC, GM, GM-CLCC N, WDS and ZT) in three replications having a total of thirty parameters. As shown in Fig. 5 B. PCA explained a total variance of 65% with PC1 contributing to 51.7% and PC2 contributing to 13.3% respectively. The seven treatments has been found to aggregate into de nite clusters displayed as elliptical circles over the ordination planes, with the larger symbols in centre of each ellipse representing the mean of three replications. In the rst (

Discussion
Impact of resource conservation on soil physical properties In the present study, higher pH was recorded under green manuring and zero tillage treatments, as compared to other treatments. Addition of Sesbania and rice residues increased the soil pH and thereby reduces the exchangeable acidity (Opala et al., 2012). Exogenous application of manure might buffer the soil acidity which changed the soil pH to a slightly higher value by defusing some free H + ions (Kumar et al., 2017). Chemical fertilizers have acidifying effects that decrease in soil pH of conventional practice (Hati et al., 2008).

Impact of resource conservation on soil carbon and nitrogen fractions
Total organic carbon (TOC) was recorded higher in organic amendment treatments (GM, BM, ZT and BC) compared to CC. Combined application of inorganic fertilizer and manure enhanced the TOC under paddy soil environment (Mohanty et al., 2013;Dossou-Yovo et al., 2016;Kumar et al., 2017) .
Our ndings also showed that resource conservation practices have higher microbial biomass carbon (MBC) content compared to CC (Table 2). Balanced nutrient inputs and supplemented by resource conservation practices play a crucial role for enhancement of soil organic carbon (SOC) and MBC (Cookson et al., 2007;Balachandar et al., 2014). The higher content of MBC in green manuring treatment might be due to presence of higher shoot and root biomass turn-  over (Mandal et al., 2007;Liu et al., 2013;Shahid et al., 2017), which signi cantly increases carbon input (Manna et al., 2005;Lal, 2015). Soil microbial biomass carbon also controls nutrient cycling soil organic matter decomposition, thereby plays a vital role in sustaining soil health. Green manuring and rice residue provide a potent source of C nutrients that facilitates the growth of soil microorganism.
Our ndings also showed that resource conservation practices have higher microbial biomass carbon (MBC) content compared to CC (Table 2). Balanced nutrient inputs and supplemented by resource conservation practices play a crucial role for enhancement of soil organic carbon (SOC) and MBC (Cookson et al., 2007;Balachandar et al., 2014). The higher content of MBC in green manuring treatment might be due to presence of higher shoot and root biomass turnover (Mandal et al., 2007;Liu et al., 2013;Shahid et al., 2017), which signi cantly increases carbon input (Manna et al., 2005;Lal, 2015). Soil microbial biomass carbon also controls nutrient cycling soil organic matter decomposition, thereby plays a vital role in sustaining soil health. Green manuring and rice residue provide a potent source of C nutrients that facilitates the growth of soil microorganism.
Resource conservation treatments enhances mineralization rate (C and N), by enhancing microbial growth and thereby enhanced the decomposition of crop residues (roots and stubbles) in the soil (Muhammad et al., 2014). Incorporation of green manuring and brown manuring, adoption of zero tillage improve soil aggregation and aggregate associate carbon, thereby facilitating SOC build up (Gupta et al., 2014;M.-Y. Liu et al., 2014;Shahid et al., 2017).
The green manuring provided a simple form of organic C to sustaining the microbial growth and have potential for maintaining higher level of MBC (Mandal et al., 2007). Microbial biomass (C, N and P) increased signi cantly with the addition of leguminous residue has low C:N ratio as compared to crop residue has reach high C:N ratios (Weber et al., 2008;Yu et al., 2015).

Impact of resource conservation on Soil enzymatic activities
Compared to rice residue, green manuring can easily decomposed by the soil microorganisms to produce simple sugar compounds, which enhances soil enzyme activities (Bhattacharyya et al., 2012). Dehydrogenase activity mostly depends on the soil microbial respiration, highest activities of which occurred under green manuring treatment also recording highest microbial population. Higher C, N substrate level (Bhattacharyya et al., 2013b) and microbial population (Kumar et al., 2017) in green manuring plots, might have promoted the soil enzymatic activities. More organic matter in amended soil contributes more C source for microorganisms resulting in higher C-mineralization and enzymatic activities .

Effect of resource conservation technology on microbial population
The population of total aerobic heterotrophic bacteria (AHB), fungi, and actinomycetes were signi cantly higher in resource conservation practices than that of control, which publicized that some speci c individual nutrients (Ramirez-Villanueva et al., 2015) present in RCTs treatments might have increased total soil microbial populations. Long-term resource conservation practices in rice soil enhance fungal and bacterial populations due to favourable substrate base (Six et al., 2006). Organic amendments provide necessary C, N and energy for microbial growth and reproduction (Huang et al., 2010). Organic manure applications signi cantly changes bacteria, actinomycetes and fungi population in soils as compared to the soils treated with mineral fertilizer (Dong et al., 2014).
Effect of resource conservation technology on microbial diversity Several investigations use to nd out the functional diversity of soil-microbes in rhizosphere using Biolog ® eco-plates . The variation in the microbial community functions due to their different metabolic activities were indicated according to optical density (OD) values (colour change) at every reaction holes that utilizes 31 kind of different C-sources (Calbrix et al., 2005). The sigmoid curves of AWCD were found in all the treatments except control in all the incubation period (i.e. 0-120 h), almost resembles the S-arch of bacterial growth (Guanghua et al., 2008), which indicated that the richness of microbial communities (Zhong and Cai, 2007) in those treatments, however, the conventional control treatment having linear curve indicated the low microbial richness (Guanghua et al., 2008).
In the present study, the increasing average well color development (AWCD) values under the different treatments was in the order of GM > GM-CLCC-N > BM > ZT > BC > WDS > CC. The highest rate of AWCD observed in green manuring and the lowest was under CC could be due to increased soil microbial biomass (C, N and P) in GM that enriched the biomass addition and microbial activities (Gu et al., 2009). Combined application of most diverse resources of organic + mineral fertilizers could greatly increase in microbial biomass and their activity which enhances nutrient availability in soils (Chang et al., 2016). It was also recommended that adjustment of the appropriate proportion of speci c organic amendments such as farmyard manure, green manure, rice straw, etc. can enhance the fertility through shifting of microbial community in rice soil under different fertilization practices (Wanjiru et al., 2015).
The higher metabolic activities of active microbial communities utilizing the C-substrates within 48 h, resulted the decrease in the rate of AWCD after 48 h of incubation in different resource conservation treatments. Since, the metabolic activity was reduced under all the treatments after 72 h; hence the analysis of soil microbial functional diversity was done at this particular time. Signi cantly higher AWCD in green manuring treatment compared to other treatments indicated that addition of biomass (green manure, rice residue, biochar) played crucial role in microbial dynamics and also shifting the soil microbial community structure. Shannon index of green manuring treated plots was signi cantly higher (p ≤ 0.05) which implied that the species richness and evenness of soil microbial communities in that particular treatment might be different from other treatments. The increasing order of Shannon index in GM, GM+CLCC-N and BM indicated that soil microbial communities were affected by biomass addition which accounts for rapid increase in microbial population (Baldrian et al., 2012) rather than their diversity (Guanghua et al., 2008;Moharana et al., 2012;Nayak et al., 2012). Resource conservation treatments could enhance the accumulation of organic which altered the pattern of potential carbon utilization and increased the Shannon, McIntosh and AWCD indices values (Chinnadurai et al., 2014). The biplot analysis (Fig. 5A) indicated the separation of RCT treatments (biomass added) from WDS and conventional control (chemical fertilizer) treatment which supported that treatments receiving green manuring, brown manuring, rice residue and biochar could have a greater in uence on microbial functional diversity than conventional control.
It has been observed that the utilization of six major carbon groups by microbial communities within and between different treatments showed a unique pattern. Consumption of carbohydrates, amino acids and carboxylic acid were higher with application of green manuring and brown manuring, which indicates that microorganisms present in that treatments were more active towards easily decomposable carbon sources than other treatments. Addition of Lupin green manure (organic N source) resulted in signi cantly higher microbial biomass and activity as compared to control soils (Preethi et al., 2013). Kumar et al. (2017) reported that at the early stages, microbial communities utilized simple sugars as major substrates, whereas complex C-substrates were utilized at later stages, which indicated that shifting of the microbial community based on presence and/or absence of available nutrients. However, microbes utilize complex C substrates (phenolic compounds, amines, polymers) more in control due to less microbial activities . Variation in Biolog patterns was mainly due to applications of different biomass and could be explained by the second quadrant and third quadrant of principal components (PCs). The present study revealed that resource conservation (chemical fertilizer + organic matter) practices signi cantly enhanced the soil biological-activity which promoted the microorganisms to utilise the different C sources.

Correlation and Stepwise regression of microbial indicators
Highly signi cant positive correlations existed among MBC with soil enzymatic activities and microbial populations, which suggested that MBC content, increased simultaneously to give rise to enzymatic activities and microbial population in the soil. The enzyme activities were highly correlated with C/N fractions; microbial populations, Shannon index and McIntosh index because their activities were increased considerable by increasing addition of labile N and C source (Bhattacharyya et al., 2013a;Zhu et al., 2014;Chaudhary et al., 2017).
The AWCD, Shannon index and McIntosh were highly correlated with microbial biomass (C, N & P), enzymatic activities and microbial populations, whereas, they were not correlated with each other except AWCD (Table 4). Shannon index provides information about the spread/distribution of C source utilization by microbes and affected more by species richness Guo et al., 2016;Tautges et al., 2016). Our study suggested that the decreased in Shannon index was due to dominance of common species of microorganisms as well as MBC, MBN and MBP which were increased along with the increasing C min in the green manuring treated soil.

Conclusions
This study demonstrated the Biolog based technique to differentiate the functional soil microbial diversities under different resource conservation practices. The present study is implying that microbial community present in biomass amended treatments (GM, GM-CLCC N, BM) utilize available or simple form of carbons for their growth (carbohydrates, amino acids and carboxylic acid), whereas microorganisms prevalent in the treatments of chemical fertilizers alone preferably utilize stable C compounds (phenolic compounds, amines, polymers) due to unavailability of labile C sources. It indicates that biomass amended treatments (GM, GM-CLCC N, BM) could supply good amount of labile C sources on real time basis for microbial activity that may protect the stable C fraction in soil, hence could support higher build-up of C in long run. Therefore, various resource conservation practices that enhance the microbial biomass, enzymatic activities and diversity at the same time maintaining or enhancing the yield need to be adopted suiting to the local condition.
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