Integrated Land Reclamation as the Basis for Enhancing Agricultural Crop Productivity (1978)

Primary Source: Afanasik G. I., Piatnitski V. N., Shaban N. S., Tribis V. P., Avdeev L. B. Integrated Land Reclamation as the Basis for Enhancing Agricultural Crop Productivity // Proceedings of the Academy of Sciences of the BSSR. Agricultural Sciences Series. — Minsk: “Nauka i Tekhnika”, 1978. — No. 4. — P. 52–58.
Institution: Belarusian Research Institute of Land Reclamation and Water Management (BelNIIMiVH).
UDC: 626.86 : 631.6

Targeted regulation of environmental conditions to optimize plant vital factors has always been at the core of land reclamation science and practice. However, traditional hydraulic reclamation systems historically remained restricted to one-dimensional water table management. This foundational paper substantiates a systemic transition toward multi-factor, computer-controlled regulation of water, air, thermal, and nutritional regimes on peat soils.

1. Limitations of Single-Factor Regulation and Nutrient Decoupling

The traditional metric used to evaluate water adequacy was the mean soil moisture content within the root-inhabited layer. However, at shallow groundwater depths (up to 1.0–1.4 m), this index proved deeply flawed: it cannot guarantee optimal plant nutrient uptake even when sufficient mineral fertilizers are applied.

During rainless periods, drying of the upper peat horizon forces root water absorption to shift into deeper horizons devoid of available nutrients. Crop biomass accumulation drops markedly. This decoupling is especially severe during periodic sluicing (sub-irrigation): raising water levels to combat drought frequently triggers a 30–40% loss in grain yield (Table 1) due to oxygen deficiency in over-saturated lower horizons and root chilling.

Optimal conditions are achieved only when the maximum of the root water absorption curve coincides precisely with the soil horizon harboring maximum available nutrients, while local moisture values remain strictly within aerobic limits.

2. Stationary Lysimetric Experiments with Groundwater Dynamics

Long-term lysimeter experiments conducted by BelNIIMiVH evaluated how controlled fluctuations in groundwater levels (GWL) govern barley productivity (Table 1).

Table 1. Dependence of barley yields on groundwater level regimes

Year Trial Variant Barley Yield, g/m2 Notes
straw grain
1969 Constant GWL H = 0.5 m 353 309 Lysimeters 2 × 2 m
Constant GWL H = 0.7 m 309 293
Constant GWL H = 1.0 m 430 362
Monotonic seasonal decline from H = 0.5 to H = 1.2 m 666 556 Dry year
Abrupt 3-day water table rise from H = 1.2 m to H = 0.5 m 525 305 45% yield reduction due to abrupt flooding
1976 Monotonic seasonal decline from 0.6 to 0.95 m 688 Lysimeters 1 × 1 m, dry season
Temporary rise to H = 60 cm during peak vegetative growth 516
1977 Monotonic seasonal decline from 0.6 to 0.95 m 712 Lysimeters 1 × 1 m, wet season
Temporary rise to H = 60 cm during peak vegetative growth 672
Same temporary rise during grain filling 673

The trials unambiguously proved that sudden water table elevations during crop development impair cereal yields. Highest yields are secured through smooth, natural receding of water tables matching downward root penetration.

3. Mathematical Modeling of Heat and Mass Transfer in the Soil-Plant-Atmosphere Continuum

To eliminate conflicting environmental factors, BelNIIMiVH developed mathematical models for the transfer of moisture, heat, gases, and dissolved salts, resolved numerically via mainframe computers. This allowed predictive charting of moisture and temperature profiles alongside active root absorption zones.

Subsequent models conceptualized the entire biophysical system: “groundwater — soil — plant — surface air boundary layer”. By solving two-dimensional moisture transfer equations across saturated and unsaturated zones, they accurately forecast transpiration rates and plant water chemical potentials.

4. Automated Experimental Proving Grounds of BelNIIMiVH

These theoretical concepts were materialized across dedicated testing grounds in Belarus:

  • Polesian Experimental Peatland Station (POBS, Luninets):
    • Commissioned in 1978: an automated sprinkling sector (11 ha) driven by programmatic timers and in-situ soil moisture thresholds;
    • Operating since 1975: a vertical tube-well drainage sector (400 ha) capable of lowering regional water tables while reusing pumped groundwater for topsoil sprinkler irrigation;
  • “Lesnoye” Sovkhoz (Kapyl District): Joint testbed with the Moscow Hydro-Reclamation Institute for automated sprinkler and drainage control;
  • “Kalinovka” Site (Lyuban District): A 40-hectare tract featuring underground water reservoirs and forced mechanical aeration of the peat root zone;
  • Telemetry Instrumentation: Jointly designed with the Agrophysical Research Institute (Leningrad), featuring automated data-logging stations capturing micrometeorological and soil-plant parameters.

5. Multi-Factor Crop Yield Performance

Yield responses achieved by transitioning from conventional agronomy to comprehensive multi-factor regulation are detailed in Table 2.

Table 2. Crop yields under varying degrees of environmental factor regulation, c/ha

Experimental Treatment Yield, c/ha (centners per hectare)
Perennial grass hay Barley grain Potato tubers
Natural background with recommended PK doses 75.9 / 102.1 56.8 / 37.2 480 / 247
Same + supplemental mineral nitrogen fertilization 108.8 / 139.5 54.3 / 39.6 526 / 260
Same + nitrogen and automated sprinkler irrigation 128.2 / 150.8 52.7 / 35.9 652 / 298
Same + peat sand mulching (thermal optimization) 134.8 / 152.2 55.2 / 37.2 648 / 340

Note. Numerator: dry 1976 season; denominator: wet 1977 season. Plot area 36 m2, fourfold replication.

Comprehensive regulation boosted perennial hay yields to 150–152 c/ha of dry matter (15 t/ha) and potatoes to 648–652 c/ha. The study confirmed that targeted factor compensation (such as offsetting drought-induced nitrogen starvation via automated micro-sprinkling) provides an indispensable tool for programmed high-yield crop cultivation on peat soils in Belarus.

6. Original Article in Belarusian

Р. І. АФАНАСІК, У. М. ПЯТНІЦКІ, М. С. ШАБАН, В. П. ТРЫБІС, Л. Б. АЎДЗЕЕЎ

КОМПЛЕКСНАЯ МЕЛІЯРАЦЫЯ — АСНОВА ПАВЫШЭННЯ ЎРАДЖАЮ СЕЛЬСКАГАСПАДАРЧЫХ КУЛЬТУР

Накіраванае рэгуляванне ўмоў знешняга асяроддзя месцазнаходжання раслін з мэтай аптымізацыі іх фактараў жыцця было заўсёды ў цэнтры ўвагі меліярацыйнай навукі і практыкі…

[The complete Belarusian original is preserved in the corresponding Russian edition].

7. References

  1. Shaban N. S. et al. Soil Science (Pochvovedenie). — 1975. — No. 7.
  2. Gilis M. B. Rational Methods of Fertilizer Application. — Moscow, 1975.
  3. Demidenko D. M. Land Reclamation and Water Management. — Minsk, 1978. — Issue 1.
  4. Afanasik G. I. Reclamation of Peatlands and Their Agricultural Utilization. — Minsk, 1977.
  5. Nerpin S. V., Chudnovsky A. F. Energy and Mass Transfer in the Plant-Soil-Air System. — Leningrad, 1975.
  6. Afanasik G. I. Reclamation of Waterlogged Soils. — Minsk, 1974.
Belarusian Research Institute of Land Reclamation and Water Management (BelNIIMiVH).
Manuscript received February 15, 1978.