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    <responseDate>2026-10-13T10:41:21Z</responseDate>
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    <identifier>10.57760/sciencedb.35113</identifier>
    <datestamp>2026-04-30T08:49:48Z</datestamp>
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<oai_dc:dc xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:date>2026-04-30</dc:date>
  <dc:title>Data for: Spatiotemporal reorganization of soil aggregates driven by film mulching in drylands: A CoDA-SBP framework reveals spatially decoupled evolutionary pathways</dc:title>
  <dc:identifier>doi:10.57760/sciencedb.35113</dc:identifier>
  <dc:language>en</dc:language>
  <dc:description>1. Data Generation Process, Processing Methods, Equipment, and ToolsGeneration Process: The dataset was obtained from a field-based stationary experiment. The experiment was conducted in an agricultural field with a history of over a decade of uniform drip-irrigated film-mulched cotton cultivation, utilizing a randomized complete block design (4 replicates). Two treatments were established: film mulching (FM; 0.01 mm transparent polyethylene film, configured with one film covering three drip tapes and six rows) and a bare-soil control (CK). Undisturbed soil samples were collected during key phenological stages of cotton growth and transported to the laboratory for processing.Processing Steps: Water-stable aggregates were determined using a standard wet-sieving method. Air-dried soil samples were slowly submerged in deionized water until fully saturated, and then transferred to a nested sieve assembly (apertures: 2, 1, 0.5, 0.25, and 0.106 mm). The sieving system was vertically oscillated at a frequency of 30 cycles/min with an amplitude of 38 mm for 30 minutes. Subsequently, the different size fractions were collected and oven-dried at 105 &amp;deg;C to a constant weight.Data Processing and Analytical Methods:Fraction merging: Because the &amp;gt;2 mm fraction had negligible mass in most samples, it was merged with the 1&amp;ndash;2 mm fraction to ensure statistical stability. Ultimately, soil aggregates were classified into five size fractions: &amp;gt;1 mm, 0.5&amp;ndash;1 mm, 0.25&amp;ndash;0.5 mm, 0.106&amp;ndash;0.25 mm, and &amp;lt;0.106 mm.Compositional Data Analysis (CoDA): To address the &amp;quot;constant-sum constraint&amp;quot; (closure problem) inherent in mass proportion data, the Aitchison geometry framework was introduced. By constructing a sequential binary partitioning (SBP) matrix, the five components were transformed into four orthogonal isometric log-ratio (ILR) coordinates with defined pedological interpretations for subsequent statistical inference using linear mixed-effects models (LMMs).Equipment and Tools Used:Hardware: Aggregate analyzer, standard nested sieves, 105 &amp;deg;C drying oven.Software platform: R 4.3.2 (core dependent packages include zCompositions for zero-value imputation, compositions for CoDA transformation, lme4 and lmerTest for LMM analysis, and emmeans for marginal mean comparisons).2. Spatiotemporal Information and ResolutionTemporal Information: Covers two consecutive full cotton growing seasons from 2024 to 2025.Temporal Resolution: Consists of 6 observation time points (Time 1 to Time 6), corresponding to the seedling, flowering-boll formation, and harvest stages over the two years. This temporal scale captured 15 cumulative hydrological (wetting-drying) events.Spatial Information: Fukang Desert Ecosystem Observation and Experiment Station, Chinese Academy of Sciences (FDEOS, 87&amp;deg;45&amp;prime;&amp;ndash;88&amp;deg;05&amp;prime; E, 43&amp;deg;45&amp;prime;&amp;ndash;44&amp;deg;30&amp;prime; N).Spatial Resolution:Vertical depth: Covers 4 specific depth intervals (0&amp;ndash;10, 10&amp;ndash;30, 30&amp;ndash;60, and 60&amp;ndash;100 cm).Horizontal micro-positions: Divided into 3 functional micro-zones based on the drip tape and film configuration. Pos A (under-mulch drip core zone, high water and nutrient flux); Pos B (under-mulch inter-drip convergence zone, overlapping lateral infiltration area); Pos C (inter-mulch bare zone, exposed to a non-covered environment, exclusive to the FM treatment).3. Data Table Structure (Record Count, Variable Labels, and Units)Record Count: The core dataset contains a total of 480 independent experimental records. (Calculation basis: The CK treatment includes two micro-positions, Pos A and Pos B, yielding 2 positions &amp;times; 4 depths &amp;times; 6 time points &amp;times; 4 replicates = 192 samples; the FM treatment includes three micro-positions, Pos A, Pos B, and Pos C, yielding 3 positions &amp;times; 4 depths &amp;times; 6 time points &amp;times; 4 replicates = 288 samples).Row Meaning: Each row in the data table represents the complete physical structural attributes of an independent undisturbed soil sample collected at a specific time, depth, and micro-position.Column Labels and Units:SampleID: Sample identifier.Block: Randomized block / experimental replicate number (1 to 4).Plot: Plot identifier.Time: Time point (1 to 6).Treatment: Treatment identifier (FM = film-mulched drip irrigation, CK = bare-soil control).Position: Horizontal functional micro-position (Pos A, Pos B, Pos C).Depth: Soil layer depth (0-10, 10-30, 30-60, 60-100), Unit: cm.Frac_&amp;gt;1mm to Frac_&amp;lt;0.106mm: Mass proportions of the 5 aggregate size fractions, Unit: %.4. Missing Data and Data ImputationUnbalanced Structure due to Experimental Design: The dataset does not contain missing values in the conventional sense (e.g., from sampling or recording errors). However, users should note that data for Pos C (the inter-mulch bare zone) exist exclusively within the FM treatment, as this micro-position division does not apply to the CK treatment (which is entirely bare soil). This inherently unbalanced design was scientifically addressed in our statistical analyses using two-stage linear mixed-effects models (Two-Stage LMMs).Zero-values handling: In extremely rare cases where the mass proportion of a specific size fraction was recorded as &amp;quot;0&amp;quot; within the compositional data, these true zeros were strictly imputed using a non-parametric replacement method (via the zCompositions R package) prior to calculating the ILR coordinates. This was done to satisfy the mathematical requirements of logarithmic transformations.5. Error Assessment and MitigationSpatial Heterogeneity Control: Point-source drip irrigation in arid regions induces steep micro-environmental gradients. To manage this, our dataset explicitly converts the heterogeneity-induced error driven by these micro-gradients into a fixed effect (Position). Furthermore, random background field noise was effectively isolated using a mixed-effects model with nested block structures (Block &amp;times; Treatment).6. File Description The repository contains 1 core data file:soil_data.xlsx: Contains the basic environmental and spatial information for all 480 samples, along with the raw mass proportion data of the water-stable aggregates across the 5 size fractions.</dc:description>
  <dc:subject>Soil water-stable aggregates; Compositional data; Film mulching</dc:subject>
  <dc:creator>Wang Ning</dc:creator>
  <dc:rights>RESTRICTED</dc:rights>
  <dc:type>dataset</dc:type>
  <dc:publisher>Science Data Bank</dc:publisher>
</oai_dc:dc>

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